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Review

Climate Zoning for Buildings: From Basic to Advanced Methods—A Review of the Scientific Literature

Department of Civil and Environmental Engineering, School of Engineering and Digital Sciences, Nazarbayev University, Astana 010000, Kazakhstan
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Author to whom correspondence should be addressed.
Buildings 2023, 13(3), 694; https://doi.org/10.3390/buildings13030694
Submission received: 29 January 2023 / Revised: 22 February 2023 / Accepted: 28 February 2023 / Published: 6 March 2023

Abstract

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Understanding the link between the energy-efficiency of buildings and climatic conditions can improve the design of energy-efficient housing. Due to global climate change and growing requirements for building energy-efficiency, the number of publications on climate zoning for buildings has grown over the last 20 years. This review attempted to give the reader an up-to-date assessment of the scientific literature in the field of climate mapping for buildings on a global and national scale, filling in the gaps of previous works and focusing on details that were not presented before. There were 105 scientific sources examined. The most dominant climate zoning variables were thoroughly analyzed. A clear categorization of climate zoning methods with specific criteria was shown. The most used methods were evaluated, emphasizing their similarities and differences, as well as their essential components and advantages. The main literature review was supported with bibliometric and bibliographic analysis. The existence of many climate zoning methods can be an indicator of the lack of agreement on the most effective strategy. A tendency has been established for the popularization among scientists of methods based on machine learning and building energy simulations, which are relatively easy to use and have proven to be the most reliable climate zoning methods. A transformation is emerging by shifting from a climate-based to a building performance-based climate zoning approach.

1. Introduction

People are becoming more conscious about the link between energy use and environmental impacts as global warming and climate change progress more significantly [1,2]. The present energy-related greenhouse gas (GHG) emissions are around 39 Gt CO2 equivalent, according to the International Energy Agency. The building industry was directly or indirectly responsible for nearly 50% of global energy consumption and 39% of total GHG emissions in 2018 [3]. While developed countries have taken significant progress to reduce their energy consumption, the energy demand for buildings rose by over 20% between 2000 and 2017 due to factors including the rapidly expanding floor area of dwellings, the relatively small reduction in energy intensity, and the rising energy requirements of the energy services [4]. Existing and future buildings will be largely responsible for determining global energy consumption [5,6,7,8,9,10]. Future growth in energy use and accompanying emissions is prominent. The increased access of billions of people in developing countries to decent housing, electricity, and improved cooking facilities is a significant trend. By 2040, buildings are expected to be the most significant source of GHG emissions [11]. In addition to the issue of climate change, there are important economic reasons why energy-efficient buildings are becoming increasingly attractive. There are between 100 and 150 million people in developed countries that are unable to afford the cost of energy due to low incomes [12]. In 2018, nearly 13% of Europeans said they live in homes that are too cold, and 20% said they live in homes that are not properly protected from the heat [13]. In 2022, the situation worsened, and wholesale electricity prices rose significantly in many countries, especially in Europe. Power prices in the first half of 2022 were more than four times as high as the average in the first half of 2016 to 2021, primarily due to gas prices climbing to more than five times the value of the reference period [14]. Therefore, during seasons of extremely high or low ambient temperatures, low-income households might confront significant heating, cooling, and health difficulties. Indeed, buildings represent a critical piece of a low-carbon future and a global challenge for integration with sustainable development. Therefore, reducing the energy and GHG footprint in both existing and new buildings represents a key challenge and an opportunity to tackle global warming and energy safety.
Building energy consumption, in turn, is influenced by several elements, where environmental or climatic factors are one of the most important [15]. With other factors (socioeconomic conditions, occupant behavior, energy management, and building design) being equal, changes in climate characteristics affect building energy consumption [16,17,18,19]. A wide range of climate variables influence buildings’ thermal performance [20,21]. The impact of climate variables is different in different geographic regions. Increasing energy-efficiency is a key goal for the building sector, and the use of climatic zoning for buildings (CZB) as a tool in the establishment of design guidelines that address lower energy consumption is an important factor to consider. However, climatic zoning (CZ) methods are diverse and there is no “standard” technique for CZB, although some are widely acknowledged and implemented [22,23,24]. It is also known that not all existing CZB approaches are directly related to building energy consumption [25,26,27].
Recognizing the relationship between the power consumption of buildings and climate conditions can help with the engineering of climate-appropriate dwellings for various geographical locations [28]. The relevance of precise CZ for building energy consumption is demonstrated by the fact that discrepancies in CZB led to a significant increase in heating and cooling energy needs [29,30]. The design of the buildings should be maximized to take into account regional priorities. Defining climate zones makes it feasible to identify and prevent the negative effects of the environment on buildings by identifying basic zonal construction criteria [31,32]; additionally, this makes it possible to support the efficient use of resources [33]. Over the past 20 years, the number of publications on CZB and the interest of scientists has increased significantly due to global climate change and higher requirements for the energy-efficiency of buildings [22,23,24,25,27,34,35,36,37,38,39,40,41,42,43,44,45,46,47,48,49,50,51,52,53,54]. Recently, numerous measures of energy-efficiency and sustainability, specifically LEED, BREAM, VERDE, and Passivhaus certificates, have demonstrated an inclination toward integrating environmental criteria into buildings [55,56].
Two review articles on CZB were identified in the analyzed literature [16,24]. Walsh et al. [38] reviewed the domestic and international standards, laws, scientific journals, and other documents about the climatic categorization of buildings and energy-saving measures implemented by 54 countries. Mainly using data from national and international building codes (90% of the cases were related to normative documents), methodologies for CZB were explored country by country. In addition to a more modern set of sources (51% of the publications we reviewed were published between 2017 and 2022), this review is different since it is focused on studying only scientific publications in the narrow field of CZB. The purpose of this study is to review academic publications in the CZB field to quantify the research output and current progress supported with bibliometric and bibliographic analysis. Additionally, a revised criterion for determining CZ methods, which was re-established with two new techniques, was used. We attempted to give the reader an up-to-date assessment of the scientific literature, filling in the gaps of previous works and focusing on details such as primary sources of climate data, its form, and the period of observation of the climate, which was not presented in Walsh’s review. Verichev et al. [16] investigated the most-cited climate-related studies in building from 1979 to 2019. One hundred twenty-eight publications were used in this paper, all with more than 35 citations. The studies were investigated by employing both manual and bibliographic analysis. This paper covers a wide range of topics, both directly and indirectly linked to climate, climate zones, and buildings. However, the author deals with the issue of the climate component for buildings only in a small part of the article. Conversely, this review is purely focused on the CZB, its methods, variables, and their impact on the building’s energy usage. To summarize, this study is unique in the following ways:
  • The information on the CZB from scientific publications in 37 countries and 95 affiliations was collected and reviewed. The Scopus database was selected as a primary source of publications. Research articles represent 84% of the materials we analyzed, while conference papers account for 10%;
  • This study is state-of-the-art since 51% of the publications reviewed were published between 2017 and 2022;
  • The study essentially differentiates buildings’ CZ variables and buildings’ CZ methods, which were typically bundled in previously published works. Each of the categories was extensively reviewed and analyzed;
  • An organized categorization of the most commonly used building CZ variables and building CZ methods (with criteria used in determining each method) is presented. The most commonly used CZB methods were evaluated emphasizing their similarities and differences, as well as their essential components and advantages. The current development of this field was explored and traced;
  • Several additional machine learning (ML) methods for CZB have been revealed. In light of this, the category of conventional clustering techniques was expanded and given a new term, “Machine Learning Methods” (MLM). Additionally, a previously rare term, “The Interval Judgment Method” (IJM), has been put into use;
  • Covering the gaps of prior works and concentrating on information that was not previously published, the primary sources of climate data and the form in which climate data are commonly used were recognized. The data on climate observation periods for CZB methods were also collected and analyzed. Other details such as the most commonly used software for energy simulations and the number of archetypes were mentioned;
  • All collected data are shown in the condensed table with the following extracted features: sources, publication years, authors, publication type, country or region of study, CZ methods used, their number and combinations, number of climate zones, etc.
  • Several promising studies regarding future climate scenarios in CZB were identified. In this review, 12% of publications dealt with future CZ, and their main principles are given;
  • Using bibliometric and bibliographic analysis for evaluating and analyzing the performance of research activities, this paper indicates substantially contributing authors, nations, the co-citation and bibliographic coupling networks, the direct citation network, etc.

2. Brief Historical Background of Climatic Zoning and Its Purpose

People have attempted the climatic classification of the earth since ancient times for different purposes. Several attempts by Greek philosophers (Pythagoras, Aristotle, Plutarch, and Ptolemy) are known to map and classify the climate [57,58]. The 19th century can be considered the beginning of the modern climate classification era, with the first published maps based on temperature and, later, precipitation parameters [59]. Vegetation-based climate classifications were started by Köppen; his first scheme was published in 1900. Still, the Köppen map remains the most widely used climate classification map, which was presented in its most recent edition in 1961 by Rudolf Geiger. It is still constantly updated and refined [38]. Because the Köppen–Geiger (KG) classification is primarily concerned with vegetation growth, it is limited in formulating the link between outdoor and indoor climates, as well as how climate influences building energy consumption. In the first half of the 20th century, building codes and standards, which contained requirements for climatic protection and durability in conformity with defined climate zones, were introduced in some countries [60,61]. Over time, the requirements of building codes and standards gradually expanded. In addition to the requirements for proper weather protection and interior comfort, the guidelines for the energy-efficiency of buildings, which sufficiently depend on accurate climate classification, were introduced [62,63].

3. Methodology

3.1. Literature Review Framework

The framework of the literature review is shown in Figure 1 and is composed of the following steps:
  • General keyword-based search in Scopus database;
  • Specific keyword-based search, with refined search parameters and keywords to find the most relevant sources;
  • The composition of the final list of sources using the following criteria. The main idea of the source should be to study or propose methods for climatic zoning of the territory for the needs of energy-efficient buildings or a non-CZB article with described methods which influence CZB or can potentially be applied to its purposes;
  • Identifying and screening additional articles. The sources that were cited by an article from the shortlist became additional candidate sources. Relevant sources outside of Scopus were also identified by Google web search. Further, the candidate sources were checked following the established criteria, and the selected ones were added to the final list;
  • Criteria were established to distinguish between climate variables and CZB methods;
  • The review of each source and extraction of information on climate variables and CZB methods. Specific features (more details are included in the Data Collection section) were also extracted from the sources at this stage;
  • All data were subjected to in-depth quantitative analysis (descriptive analysis);
  • Sources cited in Scopus were subjected to basic bibliometric and bibliographic analysis to identify bibliometric networks;
  • Discussion (interpretations of the findings, directions for future research, recommendations).

3.2. Adopted Bibliometric and Bibliographic Analysis

Bibliometrics is a valuable technique for evaluating and analyzing the performance of research activities. It corresponds to scientific progress in a variety of ways, including evaluating progress, recognizing the most authoritative sources, developing the academic basis for analyzing novelties, identifying significant scientific performers, constructing bibliometric measures to evaluate academic output, and so on [64].
In this work, the bibliometric analysis supported the mail literature review with the citation analysis, an indication of research performance and collaboration identification. Techniques such as co-citation, bibliographic coupling, co-authorship, citation, and keyword co-occurrence networks were implemented; for more information about adopted bibliometric analysis principles please refer to [65,66,67,68]. For bibliometric network visualization, the VOSviewer software was used [64,68,69,70]. The results of the bibliometric analysis contributed to the following data, which were explored and incorporated into the findings:
  • A map of affiliations or public organizations which publish more articles than others in a CZB research field;
  • The top 10 most cited articles;
  • The most contributing authors in the CZB area;
  • The most popular journals for CZB;
  • Citation over time analysis;
  • The co-citation networks of researchers;
  • The bibliographic coupling network of the top 100 authors;
  • A direct citation network;
  • The network of co-occurrences of keywords;
  • The bibliometric coupling network of countries.

4. Data Collection

The Scopus database was selected as a primary source of publications. The data collection was carried out in a general-to-specific order. The search included all languages and documents for all years of operation of Scopus (until 2022). The result of a general keyword-based search was a long-list of 3622 articles. Local climate zoning (LCZ) articles were excluded from the scope of this review. After final filtering, the specific list of publications from Scopus was formed with 93 publications. During this stage, two review articles [16,24] were found, which served as additional sources of publications. Additionally, this review included a few non-CZB-related articles [71,72,73,74,75,76,77,78]. However, the methods presented there still influence CZB or can potentially be applied to its purposes. Google search was used to find possibly valuable publications outside the Scopus database; additionally, five more articles were found.
After the filtering and selection of candidate sources, the final review list comprised 105 documents. The academic literature published from 1990 onwards was reviewed to capture the most recent published findings. More than half of the publications in the final list were published after 2017. Figure 2 depicts the timeline of all papers considered in this study. The timeline has an increasing trend, with the highest number of documents published in recent years (2017, 2021, and 2022). The typology of the final list of sources is shown in Figure 3.
During the literature review, the information was gathered, which formed the basis for further quantitative analysis. All the data are shown in the condensed table (Table 1). In the following sections, the reader will be provided with information on the climate variables used for CZB, quickly highlighting their impact on building energy consumption; then, potential climate data sources and the period for climate observations will be discussed. In the final part, the essence and characteristics of each CZB method will be addressed in the order of their popularity, starting with the most frequent. In addition, information regarding combinations of methods, as well as a discussion of the benefits and drawbacks associated with each technique, will be provided.

5. Climate Variables Used for CZB

Several factors can influence building energy consumption: building location and design, occupant behavior, energy management of the building, climate, and socioeconomic and legal-related characteristics [17,18]. The issue of the energy demand of buildings is quite complex; however, speaking of the impact of climate on buildings, it can confidently be said that with other factors being equal, changes in climate characteristics significantly influence building energy consumption. A wide range of climate variables, including outdoor air temperature (AT), solar radiation (SR), relative humidity (RH), degree-days (DDs), wind (W), etc., impact buildings’ thermal performance [20]. However, specific types of buildings are influenced by climate variables differently. Climate, for example, does not affect large venue buildings’ extreme daily heating or cooling energy usage, but for commercial buildings, daily excessive heating energy consumption is closely connected to maximum and minimum AT, dry-bulb temperature (DBT), and SR [21]. In contrast, for residential buildings, only DBT has an impact. The wet-bulb temperature (WBT) is the primary impacting climatic parameter for the extreme cooling energy consumption of commercial buildings, which indicates that the combination of AT and RH influences the cooling energy consumption [21]. For many building types, the DBT significantly impacts hourly severe heating energy consumption, followed by the WBT. In contrast, cooling energy consumption is closely connected to the WBT for commercial buildings or has no apparent relationship to climate for large venue buildings [11,21]. However, the exact mechanism by which climate influences the amount of energy that buildings consume is a complicated, contentious, and highly studied topic in the scientific community [11,17,21,36,148,149,150].
This review found 99 documents with information about the variables used. The list of the main variables that were identified consists of AT, RH, DDs, SR, precipitation (Pr), W, typical meteorological year (TMY), altitude (Al), atmospheric pressure (AP), and the pressure of water vapor (PW). Building energy simulation cases were explicitly indicated as a TMY since a compilation of meteorological elements was used during the simulation, not exact variables. In the analysis, TMY was considered as a separate independent variable. Additionally, one climatic derivative (DDs) and one geographical feature (Al) were identified as separate variables. To avoid confusion, the variables indicated in the analysis are, in fact, a set of related (close) variables grouped to simplify the further analysis; see Table 2.
Ten main variables in CZB processes, and the number of variables used simultaneously, were revealed (Figure 4). As expected, AT was the most common variable, which was alone or in combination with other variables used for the CZ in 63 cases out of 99 cases (63.6%). AT and RH were the most common combination of variables among the examined documents. To simplify, DBT, WBT, temperature ranges, diurnal, seasonal, and extreme temperatures were referred to the AT category. RH was the second most popular variable. Out of 99 cases with available data on climate variables in this literature review, 40 cases using RH for climate classification were found (40.4%). DDs are also common in climate classification and were found in 30 cases (30.3%) when implemented alone or in combination with other variables. DD and DH are essentially a derivative of AT; however, these variables were mentioned separately as independent variables in cases where climate classification was based on DDs or DHs. Despite the importance of SR for CZB, its use is not so significant; it was revealed in 25.3% of cases (25 out of 99). In this review, the SR category also combines global horizontal irradiation (GHI), sunshine duration, and daily clearness index. The use of Pr as one of the variables was encountered in 25 cases out of 99 (25.3%). This is due to the use of this variable in the popular KG method [102], which uses monthly AT and Pr for classification, and due to the frequent use of this variable in hot climate countries, such as Brazil [101], the Dominican Republic [120], Chile [73], Colombia [151], Mexico [133], and the Philippines [152]. Wind component as a climate variable is not common in CZB and was found in 12 cases (12.1%) in combination with other variables. We combined wind speed, wind frequency, and wind direction under this category. TMY was found in 15.2% of cases, and Al correction in 13%.
Most often, climate classification used two variables at the same time (29.3%). The usage of only one variable or a combination of three variables was slightly less frequent, accounting for 28.3% and 22.2%, respectively. It was infrequent to use more than three variables simultaneously for CZB (Figure 5). Furthermore, when only one variable is utilized for zoning, as seen in the first bar of Figure 4, DDs and TMY are the most popular choices. AT and RH were the most common combination of two variables among the examined documents, with a significant gap between AT and SR, which was the second most prevalent combination (Figure 6).

6. Climate Data Sources

During the course of the review, several climatic data sources became evident. Most publications use data obtained from national meteorological services (60.0%). Authors also frequently use web data sources such as the WorldClim repository, EnergyPlus website, or Global Historical Climate Network Dataset (18.7%). Cases of using databases of various software were revealed in 13.3%, with the EnergyPlus database, Autodesk Green Building Studio, and Meteonorm being the most common. Climate models were used in 6.7% of cases; basically, these are publications related to future climate scenarios [51,77,97,101] (Figure 7).
The forms in which climate data are used for classification have also been identified. Monthly mean values, TMY, daily mean and hourly values are four primary data forms. Often, the data undergo some processing and can be significantly changed from the data source to the classification itself. However, the forms that provided the core for the classifications are depicted in Figure 8.

7. Period of Climate Observation

Of interest is the period of climate observations, namely the monitoring duration and the time elapsed from the end of observation to the use of data in the climate classification. Climate change makes it preferable to use the data of recent years for accurate CZ [104]. There were 71 sources identified with an indication of the period of observations. The longest monitoring time of 102 years used for climate classification was found in the article by Wan [84]. Several authors used short observation periods of up to 5 years [22,109,122]. The average climate monitoring period was 28 years. Figure 9 shows the distribution of the observation periods. Figure 10 shows a histogram of the number of years that have passed since the last observation date until the document was published. An average of 8.5 years elapses from the end of monitoring to publication, with a period from 2 to 8 years being the most common. Given the quickly changing climatic conditions, which need the use of the most appropriate, up-to-the-moment data, it is reasonable that, on average, it takes from two to eight years between the end of observations and their utilization.

8. Methods Used for CZB

Indeed, CZB is characterized by a wide variety of applied techniques. Here, a detailed analysis of the most often used methods, the number of methods utilized simultaneously, and information about authors working with specific methods will be given.
A contextual framework or a consolidated and logical system based on opinions, ideas, and values that drive the activities taken by policymakers, researchers, or other users for CZ is viewed here as a CZ method. Along with “method”, other terms such as “approach,” “technique,” “strategy,” and “mechanism” will be used to prevent lexical repetition. Based on previous studies, we classified CZ approaches with specific criteria. The criteria used in determining each method of CZB in this review are indicated in Table 3. The conventional CZ techniques list was expanded by including the IJM. The category for cluster analysis (CA) has been enhanced with additional ML techniques; accordingly, we used the new MLM term for this domain.
There were 98 sources found with information on applied CZ methods. Figure 11 shows the diversity of CZ approaches, where the twelve most commonly used methods were identified. MLM, degree-day method (DDM), and buildings energy simulations (BES) were the three most popular methods among researchers. Table 4 shows different CZB methods and the researchers working with them. It can be seen that most of the authors work with several methods. The number of methods used simultaneously is shown in Figure 12 Often, only one method is used for CZB. Of 98 cases, one approach was used in 64 cases (65.3%), a combination of two methods was used in 27 cases (27.5%), and the simultaneous use of three or more approaches was identified in 7.2% of cases (Figure 12). In addition, when only one method was used for CZB, as shown in the first bar of Figure 12, the most prevalent choices were MLM, DDM, BES, and BCM. Next, a quick summary of the main principles and key aspects of each method will be provided. A more detailed review of each CZ method will be presented in a separate article on which the authors are already working.
Machine learning methods (MLM) denote different types of multivariate data classification and segmentation algorithms that can be successfully applied for the CZ of territories for building energy-efficiency. It can simultaneously involve many climatic and geographic variables or even be combined with some building properties, avoiding oversimplification and obtaining more meaningful results [84]. Although the most common type of ML classification in the development of climate maps is CA, other various ML approaches for CZB were revealed during this review (neural networks, principal component analysis, sensitivity analysis, etc.) [39,45,52,53,72,119,133]. Accordingly, we extended this category and used the new MLM term. Still, among all possible ML methods, CA was the most frequent technique for climate classification with hierarchical, k-nearest-neighbor, and k-means clustering.
The study by Fovell et al. [95] is one of the early attempts to adopt MLM for climate zoning. The U.S. territory was divided into climate zones using principal component analysis (PCA) and hierarchical clustering (HC) with AT and Pr as the main climate variables. In total, three different candidate clustering levels (8, 14, and 25) were tested. As the most effective with a satisfactory level of detail, an option with 14 clusters was chosen. Conflicting buffer zones and cluster overlap were found as drawbacks. According to the authors, it is important to have data points outside of the research area’s boundaries that were not included in the analysis for a categorization near the study area’s borders to make the final climate classification more accurate. Stepinski and Netzel [75] attempted to classify the climate of the entire globe based on a comprehensive clustering approach. This study included 32 different clustering-based classifications. All methods were then compared with the KG classification. The authors concluded that using three climate variables (AT, Pr, and temperature range) provides the best results. About half of the climatic zones detected by clustering were accurately matched with the KG classification classes; the rest, however, differed in their climatic characteristics and geolocation. Additionally, the authors pointed out that the k-means algorithm should be preferred over the HC algorithm in the process of climate classification. Praene et al. [74] applied HC on principal components and spatial interpolation using GIS to propose a new CZB of Madagascar. As main climate variables, RH, daily GHI, and Pr were chosen. Three climate zones that correspond to dry, humid, and highland environments were derived. The authors also investigated the relationships between established CZ and the thermal comfort levels of conventional building typologies. It was demonstrated that some building types can ensure a higher yearly comfort rate and be the most effective when erected in a specific climate zone. Walsh et al. [23] performed a survey on building energy performance maps of Nicaragua. Three CZ techniques (DDs, CA, and administrative division) were compared. It was concluded that CA can provide a more in-depth understanding of CZ than other methods, but for better results, it needs to take BES into account during the development of climate maps. It was emphasized that the appropriate selection of the method plays a central role in CZ for building energy-efficiency purposes.
Given its primary advantages, MLM provides significant potential to go deeper into the CZB and acquire more reliable, previously unavailable results. One of the most important issues is data dimensionality reduction and the proper number of clusters. PCA can be applied for data dimensionality reduction and elbow method or Hubert index for solving the number of clusters problem. However, often, MLM is supplemented with other approaches, such as BES, to generate more accurate results or to evaluate them [23,34,40,44]. It should be noted that although the problem of studying climate and its classification is location-oriented [155,156], none of the found sources used the principles of spatial analysis for CZB. Spatial analysis has become a standard in many research areas (such as epidemiology, sociology, ecology, and tourism) [157,158,159], but this has not happened in the field of CZB yet. The core concepts of geographical dependency and spatial autocorrelation are founded on The First Law of Geography, which states “everything is related to everything else, but closer things are more related than distant things” [160]. Therefore, spatial objects and phenomena should be analyzed based mainly on their locations and relationships. In this way, the role of space in CZB is emphasized, and the understanding of the working and representation of space, spatial patterns, and processes is enhanced. In CZ, the recognition of the spatial dimension is expected to yield different and more meaningful results and helps to avoid erroneous conclusions [161].
Degree-days methods (DDM) are well-known techniques that have been used for decades [162]. They indicate the severity of the climate in various locations by documenting when the external AT falls below or rises above a specified temperature during a given year, necessitating heating or cooling. This method is generally defined as the sum of the temperature differences between the outdoor mean temperature over 24 h and a base temperature daily (with 18 °C as the most frequent base temperature value). The base temperature is arbitrary, but it is commonly described as the outside temperature at which heating, ventilation, and air-conditioning (HVAC) systems do not have to operate to keep the building’s internal climate comfortable. According to ASHRAE standard [163], cooling and heating degree-days (CDD, HDD) are calculated according to Equations:
H D D t = d = 1 D t (   T b T ¯ ) d +
C D D t = d = 1 D t (   T ¯ T b ) d +
where
Tb—base temperature;
+—only positive values are considered;
T ¯ —the mean value of the maximum and minimum temperatures in a given day, as shown in Equation (3):
T ¯ = ( T m a x + T m i n ) 2
Other methods for the calculation of HDD and CDD are the mean daily degree-hours method [164], UKMO approach [162], Hitchin method [165], and Schoenau and Kehrig technique [166]. It should be emphasized that except for the mean daily degree-hours method, all other DDs calculation methods are aimed to approximate the true sum of the daily outside temperature variations. Due to approximate estimations using only the maximum and minimum values of the day or monthly mean values, those methods create considerable inaccuracies [167]. Thus, if more detailed weather data, covering the hourly outdoor dry-bulb temperature of the selected region, is available for more accurate climate classification, the mean daily degree-hours method [164] is preferred over all others.
Quayle and Diaz [168] and Le Comte and Warren [169] have found that DDs are significantly connected to electricity, natural gas, and heating consumption. HDD has also been proven to be a reliable indicator of residential energy use [170,171]. Briggs et al. [140] were some the first to use DDs for climate classification. The authors proposed a new climate classification for use in characterizing the performance of energy-efficiency measures for buildings in the USA. First, according to a table composed by Strahler [172], humid/dry/marine zones were determined, and further division was carried out based on DDs, with established intervals for each zone. The authors also compared the new classification with the existing IECC 90.1-2001 system. According to the authors, the proposed classification provided a better perspective of climate, with more uniform climate zones that better characterize U.S. climates. This classification was later included in ASHRAE Standard 169-2006. Pusat and Ekmekci [85] applied DDM to the CZB of Turkey. Unlike the Turkish official CZ code, which only considers HDDs, the authors used the HDD/CDD combination (18 °C base temperature). Six main climatic zones were identified instead of the four of the national code. The authors proposed a reclassification of the country’s climate from both a heating and cooling point of view. The findings emphasized the need for the cooling loads consideration in DD climate zone classification. Katerina Tsikaloudaki et al. [81] presented an approach for defining climatic zones in Europe based on the number of DDs. The article also concludes that the most realistic classification can be obtained with the simultaneous use of HDD and CDD. Tükel et al. [50] performed the climate classification of Turkey in terms of the thermo-economic perspective utilizing the combination of DDM and MLM. Turkey’s 80 provinces were divided into five zones by fuzzy c-means clustering technique based on DDs, thermal insulation, main wall component, and fuel type. The results showed that 16 out of 80 provinces moved to a new climatic zone when the suggested CZ was compared with the existing national thermal zones. The new classification proved that Turkey’s present national CZB is insufficient, particularly in mild regions with significant cooling demands. Verichev et al. [90] used a combination of HDD with a climate severity index (CSI) to update the boundaries of climate zones in the southern regions of Chile, where three climate zones were found. After, the relative energy consumption of houses was examined for cooling and heating in the summer and winter seasons. The investigation showed that the energy expenditures for cooling the same house during the summer may vary by 50% within the boundaries of a single thermal zone. The question of whether using only the HDD method is adequate was brought up by these substantial differences in the theoretical estimation of a building’s energy consumption. Mazzaferro et al. [46] proposed a new climate zoning of Brazil. The total number of methods used in this work was seven, the largest in this review. Among other methods, the technique of enhanced DDs was proposed, where a DBT setpoint of 10 °C was used to determine DDs values. The DDs data were then divided into groups using k-means clustering. There was a total of eight fixed clusters. The authors concluded that the enhanced DDM presented considerable performance, even though it did not involve building performance data in its application. However, the authors concluded that the quality of CZ could be significantly improved by using a preliminary assessment of zoning by building performance data.
The popularity of the DDM for CZB is partly related to its ease of understanding and close connection with energy use, especially in cold regions [162]. DDM can provide quality CZ for a range of applications due to its documented relationship to building energy consumption. However, DDM operates primarily with outside AT alone, ignoring other key climatic factors that affect a building’s energy consumption. Choosing the correct base temperature is also crucial, as the incorrect base temperature will lead to inaccurate DDs [173]. Bioclimatic comfort zones, as described in [80], can be used to determine the base temperature. The DDM is the second most common method we found in CZB.
Building energy simulation (BES) has shown great potential when applied to CZB [24,25]. BES is a method of determining how a building and its components will behave in real-world scenarios. This is accomplished by using a mathematical model that simulates situations in a virtual environment. Within the framework of this review, the term is understood as the energy consumption of a building in a given climate based on the heating, cooling, and lighting loads. The climate classification procedure based on BES consists of generating performance maps showing how a set of chosen indicators, such as energy consumption or thermal comfort, vary throughout the territory (country or region) for given archetype buildings, for a typical year of climatic data. These maps are produced using building performance simulation results. The building performance is then linked to each climatic zone under study [25]. The idea of using BES for CZB is that the performance of a building model inside a single climate zone should stay essentially the same. BES is less common than DDM, but becomes more widely used in CZB applications.
Shaan Cory et al. [42] proved that for better climate classification, data on the weather and climate of the region are not enough. The authors noticed that sometimes when using external climate data for classifying climatic zones, buildings of different types could be assigned to different climatic zones during the thermal simulation within the same location. An adjustment to the traditional approach to climate classification for buildings was proposed. The authors used the climate indicator determined from the results of simulations, which was simply a three-level definition of climate challenges of building: heating-dominated, cooling-dominated, or mixed heating- and cooling-dominated. Thus, the refined classification was made based on the external climate characteristics together with the reference thermal data of the building. The authors also noted that buildings in cold regions could not be classified solely by using external climatic conditions. Walsh et al. [25,32] used BES to validate the CZB produced by other methods and reduce misclassification. The concept of the Percentage Misclassified Areas (PMA) was introduced, which is based on the idea that each climatic zone should have its unique climate conditions, which leads to a unique performance (cooling and heating energy demand) for a particular type of building. By this, there should be no overlap observed in the building performance of an identical building type placed in different zones. Results also showed the challenges of developing CZ to address multiple building types, as each archetype showed particular sensitivity to climate. Mazzaferro et al. [107] developed a data-driven CZ methodology to increase the robustness of CZB. In this study, climatic zone validation was performed by thermal loads of three different-sized office buildings as building performance indicators. An assessment was performed by comparing building thermal load results within each climatic zone obtained by clustering climatic variables (DBT, RH, and GHI). It has been proven that the utilization of BES results, data analysis, and CA methods can greatly contribute to the development of CZ methodology. In 2020, in the development of their previous study, the same team carried out work to determine the climatic zones of Brazil for building energy-efficiency regulations [46]. Climate classification was performed with known CZ methodologies (ASHRAE 169, Koppen-Geiger, Brazilian regulation method NBR 15220, Roriz method) and alternative methods (data-driven, enhanced DD, and decision tree method) supported by building performance results. The authors concluded that the quality of CZ could be greatly improved by using a preliminary assessment of zoning by building performance data.
BES is currently regarded as the most accurate method for predicting thermal building performance and has demonstrated significant promise as a policy tool [174] when applied to CZ, mainly through parametric analysis. Detailed climatic data and BES, according to several sources, could aid in the construction of a more robust climatic categorization [23,46,83,174]. However, there are certain limitations to its use in CZB, such as the necessity to pre-define a design hypothesis that differs depending on building type, occupational patterns, and HVAC systems. Furthermore, thorough meteorological data are required, which are not always available for the locations of interest [41].
Many authors use the BES method to work on the topic of the impact of climate change on buildings and CZB [89,98,111]. This is partly because simulations can be easily used to gain insight into the future energy consumption of buildings and, based on that, analyze the possible future climate zones. The data from future climate models can be easily represented as future weather files. Different methodologies and software tools can be applied [175,176]. These files are then used to simulate buildings under future scenarios.
The bioclimatic chart method (BCM) can also be used to change or create new CZ classifications. The BC analysis usually leads to identifying the possibility of passive design methods to preserve thermal comfort in outdoor spaces while also contributing to a more energy-efficient built environment. BC usually depicts the combination of AT and RH at any given time, so it becomes easier to analyze the climate features of a given location. This paper includes Givoni [177,178], Lamberts [92], Milne [179], Olgyay [180], and other psychometric chart methods in the BC category. Early attempts to develop concepts for bioclimatic building design were made by Olgyay [180]. He conducted a study on the influence of climate on building design concepts around the world and identified four major climate groups: cool, temperate, hot and arid, and hot and humid. Human tolerance ranges were also established from a BC using a combination of RH and DBT. In addition to the average radiant temperature, wind speed and SR were taken into consideration. A zone in the middle of a psychrometric chart established the range of conditions people find comfortable in different situations. Milne and Givoni [179] developed BC based on typical psychrometric charts frequently used to assess the characteristics of moist air. Additionally, four main climate categories—hot, warm–temperate, cool–temperate, and cold—were identified, along with eleven additional sub-climatic categories. The study of the effects of the environment on occupant comfort and thermal adaptability showed promising implications for the design of HVAC systems and the enhancement of building energy-efficiency. Bodach [129] proposed a foundation for creating BC zones for building design in Nepal. The psychrometric chart was used to identify passive design ideas for each location using a BC approach. Finally, a summary of building design tactics that are suited for the summer and winter in each zone was created. According to the authors, to create more climate-responsive and energy-efficient buildings, planners and architects can use proposed climate classification to make general judgments at an early design stage. Additionally, it might help with the creation of proper building energy regulations. The BCM, however, has some limitations because it only takes two climate variables into account (AT and RH). Da Casa Martin [113] offered a way for creating a CZB based on Givoni’s design principles for the Autonomous Community of Galicia (Spain), creating general zoning between five geographical regions (CZ) with comparable behavior. New climate classification could give the designers knowledge of the techniques that can be employed to establish direct recommendations and different bioclimatic strategies that can be adopted to obtain more energy-efficient buildings. New climate classification based on BCM and DB-HE-2013 code were compared to identify their similarities and differences, finding that each should have its own specific applications.
Even though the primary goal of BCs is to provide comfortable indoor conditions under thermal comfort requirements, a consequence of adopting BCM is an increase in the building’s energy-efficiency due to reduced energy demand. Additionally, a significant correlation is demonstrated between bioclimatic potential and annual building energy consumption [48,83]. Nonetheless, several resources recommend utilizing BCM in conjunction with BES [42,48,83,181] to produce secure results in terms of climatic zoning.
Köppen–Geiger method (KGM), as was mentioned, is one of the oldest and most well-established methods. A monthly record of average AT and Pr data is the only need for determining KG climatic zones. The elevational component can be taken into account in some circumstances. The KG climate map of the world is constantly updated and refined [78,102]. Based on a global data set of long-term monthly AT and Pr time series data, Peel et al. [102] used the KG method to produce a new global climate map. Climate variables were interpolated for each continent on a 0.1 × 0.1-degree grid. With each variable being interpolated separately, the updated KG world climate map was produced utilizing statistics from stations during their complete record period from 1951 to 2000. Beck et al. [77] published updated global KG climate maps with a 1 km resolution for current conditions (1980–2016) and predicted future climate change scenarios (2071–2100). The current map was made using an ensemble of four high-resolution, spatially adjusted climate maps. Particularly in regions with sharp spatial or elevation gradients, the new maps offer far more detail and classification accuracy than prior ones. Not having an unambiguous connection with CZB or energy-efficient CZ, the KGM is still used for these purposes [99,100,103]. Pernigotto et al. [99,100] discussed the application of the KGM with CA (HC) to address the issues of climate classification and representative climate identification. Results were found to be similar to KG, but the proposed climatic categories were fewer and more homogenous. Overall, KG improved by CA is intended to characterize building performance under various climatic conditions, support the creation of national or international energy policies, and give an analytical reference for CZ and the selection of representative climates.
KGM can hardly be used for precisely characterizing the performance of energy-efficiency measures for buildings. KGM alone does not allow for the accumulation of accurate data needed to address the issue of CZB. Multiple sources compared the precision of a KGM classification to that of a CA (k-means clustering) and BES, revealing that CA and BES exceed traditional KG classification quality [72,74,75].
The climate severity index method (CSIM) is capable of characterizing climate severities; accordingly, there is a wide variety of approaches to the calculation of such indices [182,183,184]. The core concept of CSI is that climate variables can be combined into a single site-specific value that defines the severity of a specific climate. The data can be examined like any other meteorological parameter to identify trends, develop sector-specific applications, and examine climate patterns or individual seasons to put their severity into context. Speaking of the CSI in this article, we mean the index used in the practice of Spain [43] and Chile [122], which uses the HDD, CDD, hours of sunshine duration, and regression coefficients for calculation. Accordingly, the summer climate severity (SCS) is determined using Equation (4), and winter climate severity (WCS) is defined by Equation (5).
S C S = a · C D D 20 j u n s e p + b · C D D 20 j u n s e p 2 + c
W C S = a · H D D 20 o c t m a y + b n N + c · H D D 20 o c t m a y 2 + d · ( n N ) 2 + e
where
CDD20(jun-sep)—the hourly sum of CDD (20 °C base temperature) from June to September;
HDD20(oct-may)—the sum of HDD (20 °C base temperature) from October to May;
n—the sum of hours of sunshine duration from October to May;
N—the sum of maximum hours of sunshine duration for October through May;
a, b, c, d, e—the regression coefficients.
In this case, SCS and WCS were produced using absolute data on heating and cooling energy consumption. The index of relative energy use for cooling and heating buildings was then connected with the climate-related values of meteorological indicators. Since CSIM is based on building energy consumption translated into conditional indices, it has a certain potential and can be applied to CZB. It is easy to establish climatic severity indices and classify the territory into climate zones using the simple formula, DD, and sunshine duration. In general, the idea of utilizing a regression model based on a number of the most crucial CZB characteristics, such as building energy consumption, DD, and SR, appears to have the potential to be successful. However, it is difficult to adapt the strategy to other regions outside of Spain because the calculation of the regression coefficients is still not entirely clear.
Other methods. The climate classification methods found during the literature review are not limited to the six methods described previously. Less popular techniques are the IJM [118,144], the frequency distribution of climate variables (FDV) [88,121] the Mahoney method (MM) [116,135], Thornthwaite climate classification (TCCM) [101], heating or cooling index (HCIM) [84], Quitt’s climate classification [112], and existing building stock performance (EBSM) [123,125].
As was previously stated, the issue of CZ has long been studied, initially predominantly for agricultural purposes and later for building and construction applications. In the first half of the 20th century, building climatology was more responsible for weather protection and interior comfort provision rather than energy-efficiency. KGM and IJM, which used a limited number of basic climate variables (AT and Pr), were then adequate [185]. Indeed, these fundamental methods were limited in their ability to incorporate a large number of climatic variables into the analysis and were far from establishing an obvious and understandable link between the variables and the energy usage of buildings. Later, during the 1970–1980s, a clear correlation was established between the main climate variables (mostly AT and its various derivatives) and the energy consumption of buildings [168,169,170,171,186,187,188]. DDs, used alongside or sometimes replacing other climate variables, started to occupy one of the leading places in CZB. At the same time, work began in the field of bioclimatic architecture, and BC were introduced [177,179]. In the early 1990s, CA was implemented in CZ with PCA, hierarchical clustering, and artificial neural networks, which can be considered as the beginning of a new stage in the development of CZB [95,119]. Over time, CA has become one of the main methods in the study of CZ along with DDM [84,87,94,96,139]. Later, experiments started on the use of BES for CZB needs, and more MLM were incorporated into this field [42,174,189]. Since the 2010s, scientists’ enthusiasm for MLM and BES has grown considerably. The possibilities of traditional and contemporary methods were extensively compared. In this way, more recent MLM and BES were interpreted with older KG, BCM, and DDM [23,25,46,100,101,103,107,122]. Recently, BES and MLM have shown great potential when applied to CZB. In addition, the significance of using BES to validate CZB was proved by several publications [23,25,46,79,83,104]. Overall, BES and MLM methods are simple to implement and have shown to be reliable in defining CZ by transitioning from a climate-based to a performance-based approach. Additionally, a combination of approaches yields much better and more robust zoning classification results. Any combination of DDM, BES, and MLM techniques is likely to be the most powerful, efficient, and promising, delivering the most consistent results. It is reasonable to claim that there is now a solid scientific basis for widely applying BES and MLM in official national CZ codes and regulations. However, the presence of so many strategies indicates that there is still no consensus about the optimal CZB strategy, emphasizing the importance of further research work in this field.
In the next section, we will support the findings of this review with bibliometrics and bibliographic analysis, which aims to indicate substantially contributing nations, affiliations, journals, authors, and connections among them. A network of keywords, articles and overall link strength among publications will be discussed. We will present the data step by step, most clearly reflecting the performance of research activities and academic output in the CZB field.

9. Bibliometric Analysis

In this work, 98 (Scopus cited) articles were subjected to bibliometric analysis. To identify the most significant affiliations or public organizations in a CZB research field and their geographical location, a map (Figure 13) was formed which indicates the affiliations in which the researchers are registered. The larger the mark on the map, the greater the contribution (number of papers published). In addition, a list of affiliations that have three or more publications in a CZB is shown; those 10 affiliations are marked on the map with signatures. Among 98 publications, the largest number of publications (six each) belong to authors from the University of Granada (Spain), Xi’an University of Architecture and Technology (China), and the Austral University of Chile.
The publications considered in this analysis had a total of 9696 citations in Scopus. Excluding two highly cited papers [77,102] concerning KG climate classification, the average citation per article of the remaining 96 articles is about 35. The top 10 most cited articles from our list are shown in Table 5. The largest number of articles was published in Energy Additionally, Buildings, Building and Environment (previously Building Science), and Energy Conversion and Management (previously Energy Conversion) journals. The list of the most significant journals is shown in Figure 14. There are eight most-contributing authors (with four or more papers): Carpio [41,51,83,109,122]; Verichev [22,51,83,109,122]; Walsh [23,24,25,32,100]; Yang [35,52,71,84,87]; Zamorano [41,51,83,109]; Attia [7,49,80,106]; Cóstola [23,24,25,32]; and Labaki [23,24,25,32]. Figure 15 shows the top 20 most contributing authors (with two or more published papers). Articles were also analyzed by citation over time. A trend line and articles cited above the trend were determined (Figure 16). This indicates an increased interest in particular articles [6,7,73,89,94,95,125,190] from the scientific community.
Since the early days of bibliometric research, the concept of visualizing bibliometric networks, often known as “science mapping” has gotten a lot of attention. Visualization is an effective method for analyzing a wide range of bibliometric networks [68]. In the next section, the results of performed bibliographic analysis will be provided.

10. Bibliographic Analysis

Co-citation analysis in this review is represented by the co-citation networks of researchers (Figure 17). To better perceive the visualization, the number of its nodes has been reduced, and the top 36 authors out of 5036 who passed the threshold level with the minimum number of citations of 15 were used for visualization. Each circle in the visualization represents an author. The size of a circle reflects the number of citations an author has received. Authors that are located close to each other in the visualization tend to be more strongly related, based on co-citations rather than authors/journals that are located far away from each other. Three clusters of most-cited authors are revealed.
  • Koppen, W.; Rubel, F.; and Kottek, M. are authors whose research topic is Köppen–Geiger climate classification in the upper left area [78,191,192,193,194];
  • Santamouris, M.; Attia, S.; Givoni, B.; and Carlucci, S. are authors that publish articles on the energy-efficiency of buildings, bioclimatic studies, and urban or local climate zoning research in the upper right area (green cluster) [7,177,178,195,196,197,198,199,200];
  • Costola, D.; Labaki, L.C.; Carpio, M.; Verichev, K.; and Yang, L. are directly focused on climate classification methods for buildings [16,23,24,25,32,41,51,83,84,90,122].
Additionally, the bibliographic coupling network of the top 100 authors (Figure 18) was created by analogy with the bibliographic coupling network of journals. Here, the closer two researchers are located to each other in the visualization, the more strongly they are related to each other based on bibliographic coupling. In other words, researchers that are located close to each other tend to cite the same publications. The network shows three groups of closely related authors:
  • Yang, L. and Walsh, A;
  • Almeida, M., Attia, S., and Roshan, G.;
  • Carpio, M., Verichev, K., and Diaz Lopez, C.
A direct citation network (Figure 19) based on articles that have at least one citation (90 out of 98) was constructed. We used normalized citations to correct the fact that older documents have had more time to receive citations than more recent documents. In VOSviewer the number of citations in a document is normalized by dividing it by the average number of citations in all publications issued in the same year and used for the VOSviewer files [70]. Using overlay visualization means that not only can a direct indication of the relatedness of publications be recognized, but the papers that have a high direct citation in this group of documents can be recognized, which indicates high interest from researchers working at the moment.
The network of co-occurrences of keywords has also been analyzed (Figure 20). The main objective here was to obtain a sense of the terms that researchers used and to see whether there were any new subtopics. Of 2433 keywords, 58 keywords that occurred more than 10 times met the threshold and were used in the analysis. Keywords were extracted from the title and abstract of publications. Here, the larger the circle, the more often a keyword appears in the title, abstract, or keyword list of publications, and the closer keywords are to each other in the network, the greater the frequency of co-occurrences of the two terms in one publication. Using overlay visualization, the average publication year of each keyword can be recognized with a differentiation of colors from purple for the average publication year around 2012 to yellow for 2018. The top three keywords were: “buildings”, “energy efficiency”, and “climate change” with 31, 31, and 21 occurrences, respectively.
Keyword analysis shows that in the area of energy-efficient buildings, the issue of climate change is becoming quite important. To design energy-efficient and climate-resilient buildings, it is critical to gain insights into the energy demand across the building’s service life from the early design stage onwards. Thirteen articles connected with climate change were found in the studied literature. However, in this article, we limit ourselves to specific information. As it becomes trendy to incorporate climate change into CZB studies, a more detailed review of this field may become the topic of our future publications. Here, we only give information about the number of publications in this review concerning future climate scenarios (Figure 21) and other details such as predicted period, climate model, and scenario type (Table 6).
In addition to the above-discussed map of affiliations or public organizations, the bibliometric coupling network of countries is shown in Figure 22. However, unlike the above-discussed map, which is based on the number of publications, Figure 22 is based on bibliographic coupling information, which is, in general, an overlap in the reference lists of publications. Here, the larger the number of references two countries have in common, the stronger the bibliographic coupling relation between the countries. All 46 countries were mapped. By analogy with the bibliographic coupling network of journals, here, each circle represents a country. Large circles represent countries that have high normalized citation weight, and small circles are countries with a low number of citations. Generally, the closer two countries are placed in the visualization, the more closely they are connected based on bibliographic coupling. A group of Spain, China, the US, Australia, and Chile has close relations, with the strongest link between Spain and Chile.

11. Discussion

In this literature review, extensive detailed data were extracted from the available documents regarding CZB. Publication years and their type, authors, country or region of study, climate variables used, climate zoning methods used and their combinations, period of climate observations, number of climate zones, and other pertinent details served as the foundation for the subsequent analysis. Climate data sources and the period for climate observations were also highlighted.
For the categorization of CZ variables and CZ methods, detailed criteria were established. Ten major variables and the number of variables employed simultaneously for CZB were found. As anticipated, AT was the most prevalent variable used alone or in combination with other variables (63.6%). AT and RH were the most often occurring combination of variables across the articles reviewed. CZB employed two climatic variables simultaneously in 29.3% of cases. The use of a single variable or a combination of three variables was marginally less common, accounting for 28.3% and 22.2% of all cases, respectively. The use of more than three variables simultaneously for climate categorization was uncommon. In addition, when only one variable was used for zoning, DDs and TMY were the most common options. AT and RH were the most prevalent pairing of two variables in CZB. Typically, national meteorological services were the source of climate data. Less often used, but still popular, were web databases and software applications such as EnergyPlus, Autodesk Green Building Studio (GBS), and Meteonorm. Climate models were used in 6.7% of cases, basically for future climate scenarios. It is preferable to use contemporary climate data (last 20–30 years) for appropriate climatic zoning due to climate change.
CZB is characterized by a wide variety of applied methods and not all of them are directly related to building energy consumption. The twelve most commonly used methods were identified. MLM, DDM, and BES were the three most popular approaches. Often, only one method was used for CZ. One approach was used in 65% of cases, a combination of two methods was used in 28%, and the simultaneous use of three or more approaches was identified in 7% of cases. In addition, when only one method was used for CZB, the most prevalent choices were MLM, DDM, BES, and BCM.
Given its primary advantages, MLM provides significant potential to go deeper into the CZB and acquire more reliable, previously unavailable results. However, often, MLM is supplemented with other approaches, such as BES, to generate more accurate results or to evaluate them.
Due to its well-documented connection to building energy, DDM can offer high-quality CZ for a variety of applications. However, DDM primarily uses the outside AT and ignores other significant climatic variables that have an impact on a building’s energy use. It should be underlined that the mean daily degree-hours technique is favored over all others for more accurate DDs calculation if more comprehensive meteorological information encompassing hourly outdoor AT of the chosen location is available.
BES is currently regarded as the most accurate method for predicting thermal building performance and has demonstrated significant promise as a policy tool when applied to CZB. Detailed climatic data and BES, according to several sources, could aid in the construction of a more robust climatic categorization [23,46,83,174].
Multiple methods can be used simultaneously as a strategy to improve CZB or validate its results. Any combinations based on DDM, BES, and MLM techniques tend to be the most powerful, efficient, and promising, providing the most reliable results. The main quality criteria of CZB assume that the energy consumption of one building archetype within one climatic zone should be nearly identical.
The dynamics of climate change are forcing scientists to predict future climate conditions and adapt buildings accordingly. To ensure the growth of a building stock that is sustainable and resilient, it is crucial to design and construct buildings today that can take on the dynamics of the environment during their entire life cycle. Several studies regarding future climate scenarios in CZB were revealed [37,51,54,97,98,109,176]. In this review, 12% of publications dealt with future climate zoning for buildings. BES can be easily used to gain insight into the future energy consumption of buildings and, based on that, analyze the possible future climate zones.
A bibliometric analysis was performed to support the main part of this review, which made it possible to evaluate and analyze the performance of research activities in the CZB field, including evaluating the scientific progress, recognizing the most authoritative journals, and identifying significant scientific performers. This evaluation and analysis were performed using bibliometric networks of co-citation, bibliographic coupling, keyword co-occurrence, and co-authorship techniques.

12. Conclusions

The energy consumption of buildings is affected by environmental or climatic conditions and varies with climate variability. Proper climate zoning is essential for most building energy-efficiency policies, with great importance in meeting growth targets for energy security and reducing GHG emissions. Thus, consideration should be given to the use of climatic zoning as a tool in the formulation of construction guidelines that address the energy-efficiency of buildings. Most sectors are implementing stricter energy-efficiency standards due to concerns over climate change and the diminishing availability of natural resources; here, CZB should be an essential factor to take into account. The ability to correctly categorize climates is fundamental to sustainable design, which can reduce the need for heating and cooling by a significant amount. Defining zones not only makes it possible to identify and mitigate the adverse impacts of climate on buildings by specifying basic zonal construction criteria, but also makes it possible to support the effective utilization of climate resources. Understanding the relationship between energy conservation and climate conditions in buildings can be beneficial to the design of housing that is climate-appropriate for a variety of geographical locations.
With this review, we set the goal of understanding at what level of scientific progress the CZB is now, and whether there have been positive cardinal changes in the study of climate zoning for buildings. We analyzed scientific publications in the field of CZB which have already been put into practice or are just being developed. In the last 10 years, there has been a significant increase in the number of publications on the CZB topic.
Now, climatic zoning approaches vary, and there is no “standard” strategy for CZB, though several are generally recognized and used. At the current stage, two global climate zoning systems are used for the needs of buildings and construction. The KG map is popular among researchers but can be hardly used for characterizing the performance of energy-efficiency measures for buildings. KG did not allow for the accumulation of accurate data needed to address the issue of CZB. Multiple sources compared the precision of a KG classification to that of an MLM and BES, revealing that ML and BES exceed traditional KG classification quality [72,74,201]. The degree-day-based global map of ASHRAE Standard, first presented in 2014, remains essentially the only solution providing data on climate zones for buildings globally. It is worth noting that, based only on degree-days, the ASHRAE map inherits its shortcomings, such as the use of outside AT and eliminating other environmental variables that affect a building’s energy consumption. Additionally, the usage of only seven main zones with rather wide intervals of degree-days can lead to simplification of zoning. The use of more advanced zoning methods such as MLM or BES is still limited to the territories of countries and continents [7,50,81,105]. The official government standards for climate zoning, especially in developing countries, are very often criticized by the scientific community for not being able to be used with high accuracy and reliability [2,27,43,47,50,53,104,142]. The introduction of a standard global climate zoning approach or map for energy-efficient buildings based on methods recognized as the most effective among scientists could positively influence the problem of energy use in buildings at the global level. This action currently appears to be reasonably realistic given the sufficiency and quality of the available climatic data on a global scale.
It was revealed that BES and MLM have shown great potential when applied to climate zoning. It is reasonable to claim that there is now a solid scientific basis for applying BES and MLM for climate zoning needs. In addition, the significance of using BES to validate climatic zoning for buildings was proved by several publications. Overall, BES and MLM methods are simple to implement and have shown to be reliable in defining climate zones by transitioning from a climate-based to a performance-based approach. Additionally, a combination of approaches yields much better and more robust zoning classification results. It can also be assumed that over the next decade, we might see the gradual introduction of MLM and BES into the official standards of different countries, which could certainly have a positive impact on the energy-efficiency of buildings in particular and may also have a positive impact on the global climate change problem.
It is important to note that uncommon methods such as EBS and FDV can be used to create new CZ or to amend and enhance existing CZ. The real energy consumption of buildings in the EBS approach is very useful information that can help to understand how certain aspects (including climate) affect a building’s final energy consumption. However, there are no publications to date that compare these methods to others to assess their quality.
Although the problem of studying climate and its classification is location-oriented, none of the found sources use the principles of spatial analysis or did not mention it. Spatial analysis has become a standard in many research areas (such as epidemiology, sociology, ecology, and tourism), but this has yet to be applied in the field of CZB. The role of the spatial aspect in CZB research is underestimated, and the understanding of the working and representation of space, spatial patterns, and processes is limited. One of the strongest future improvements in the field is the recognition of the spatial component in CZB, which has the potential to be favorable and is predicted to produce results that are more accurate and robust.

Author Contributions

Conceptualization, A.R. and S.A.M.; methodology, A.R. and S.A.M.; software, A.R.; validation, A.R. and S.A.M.; formal analysis, A.R.; investigation, A.R.; resources, S.A.M. and J.R.K.; data curation, S.A.M.; writing—original draft preparation, A.R.; writing—review and editing, A.R. and S.A.M.; visualization, A.R.; supervision, S.A.M.; project administration, S.A.M.; funding acquisition, S.A.M. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by Nazarbayev University, Kazakhstan Faculty development competitive research grants numbers 021220FD0651.

Data Availability Statement

All data collected and analyzed in this review are presented in Table 1 of this article.

Conflicts of Interest

The authors declare no conflict of interest.

Abbreviations

AlAltitude
APAtmospheric Pressure
ASHRAEThe American Society of Heating, Refrigerating, and Air-Conditioning Engineers
ATAir Temperature
BCMBioclimatic Charts Method
BESBuilding Energy Simulation
CACluster Analysis
CSIMClimate Severity Index Method
CDDCooling Degree-Day
CDHCooling Degree-Hour
CZClimatic Zoning
CZBClimatic Zoning For Buildings
DBTDry-Bulb Temperature
DDsDegree-Days
DHsDegree-Hours
DDMDegree-Days Methods
EBSMExisting Building Stock Performance Method
FDVA Frequency Distribution Of Climate Variables
GHGGreenhouse Gas
GHIGlobal Horizontal Irradiation
HCIHeating Or Cooling Index
HCHierarchical Clustering
HDDHeating Degree-Day
HDHHeating Degree-Hour
HVACHeating, Ventilation, and Air-Conditioning Systems
IJMInterval Judgment Method
IPCCIntergovernmental Panel on Climate Change
KGKöppen–Geiger
KGMKöppen–Geiger Method
LCZLocal Climate Zoning
MLMachine Learning
MLMMachine Learning Methods
MMMahoney Method
PCAPrincipal Component Analysis
PMAPercentage Misclassified Areas
PrPrecipitation
PWThe Pressure of Water Vapor
RCPRepresentative Concentration Pathway
RHRelative Humidity
SRSolar Radiation
TCCMThornthwaite Climate Classification Method
TMYTypical Meteorological Year
WWind
WBTWet-Bulb Temperature

References

  1. Li, D.H.W.; Yang, L.; Lam, J.C. Impact of climate change on energy use in the built environment in different climate zones—A review. Energy 2012, 42, 103–112. [Google Scholar] [CrossRef]
  2. van Ruijven, B.J.; De Cian, E.; Wing, I.S. Amplification of future energy demand growth due to climate change. Nat. Commun. 2019, 10, 2762. [Google Scholar] [CrossRef] [Green Version]
  3. UN Environment Programme. Global Status Report for Buildings and Construction: Towards a Zero-Emission, Efficient and Resilient Buildings and Construction Sector, Global Status Report. Available online: https://globalabc.org/sites/default/files/2022-11/FULL%20REPORT_2022%20Buildings-GSR_1.pdf (accessed on 1 May 2022).
  4. IEA. Perspectives for the Clean Energy Transition. The Critical Role of Buildings. 2019. Available online: https://www.iea.org/reports/the-critical-role-of-buildings (accessed on 1 May 2022).
  5. Tootkaboni, M.P.; Ballarini, I.; Corrado, V. Analysing the future energy performance of residential buildings in the most populated Italian climatic zone: A study of climate change impacts. Energy Rep. 2021, 7, 8548–8560. [Google Scholar] [CrossRef]
  6. Asimakopoulos, D.A.; Santamouris, M.; Farrou, I.; Laskari, M.; Saliari, M.; Zanis, G.; Giannakidis, G.; Tigas, K.; Kapsomenakis, J.; Douvis, C.; et al. Modelling the energy demand projection of the building sector in Greece in the 21st century. Energy Build. 2012, 49, 488–498. [Google Scholar] [CrossRef]
  7. Attia, S.; Eleftheriou, P.; Xeni, F.; Morlot, R.; Ménézo, C.; Kostopoulos, V.; Betsi, M.; Kalaitzoglou, I.; Pagliano, L.; Cellura, M.; et al. Overview and future challenges of nearly zero energy buildings (nZEB) design in Southern Europe. Energy Build. 2017, 155, 439–458. [Google Scholar] [CrossRef]
  8. Bell, N.O.; Bilbao, J.I.; Kay, M.; Sproul, A.B. Future climate scenarios and their impact on heating, ventilation and air-conditioning system design and performance for commercial buildings for 2050. Renew. Sustain. Energy Rev. 2022, 162, 112363. [Google Scholar] [CrossRef]
  9. Ramon, D.; Allacker, K.; De Troyer, F.; Wouters, H.; van Lipzig, N.P.M. Future heating and cooling degree days for Belgium under a high-end climate change scenario. Energy Build. 2020, 216, 109935. [Google Scholar] [CrossRef]
  10. Roshan, G.; Orosa, J.A.; Nasrabadi, T. Simulation of climate change impact on energy consumption in buildings, case study of Iran. Energy Policy 2012, 49, 731–739. [Google Scholar] [CrossRef]
  11. Li, L.; Sun, W.; Hu, W.; Sun, Y. Impact of natural and social environmental factors on building energy consumption: Based on bibliometrics. J. Build. Eng. 2021, 37, 102136. [Google Scholar] [CrossRef]
  12. Santamouris, M. Green commercial buildings save energy. Nat. Sustain. 2018, 1, 613–614. [Google Scholar] [CrossRef]
  13. WHO. Housing and Health Guidelines. 2018. Available online: https://apps.who.int/iris/bitstream/handle/10665/276001/9789241550376-eng.pdf (accessed on 22 June 2022).
  14. IEA. Electricity Market Report. July 2022—Update. Available online: https://www.iea.org/reports/electricity-market-report-july-2022/executive-summary (accessed on 25 August 2022).
  15. Bohne, R.A.; Huang, L.; Lohne, J. A global overview of residential building energy consumption in eight climate zones. Int. J. Sustain. Build. Technol. Urban Dev. 2016, 7, 38–51. [Google Scholar] [CrossRef]
  16. Verichev, K.; Zamorano, M.; Salazar-Concha, C.; Carpio, M. Analysis of Climate-Oriented Researches in Building. Appl. Sci. 2021, 11, 3251. [Google Scholar] [CrossRef]
  17. De Silva, M.N.; Sandanayake, Y.G. Building energy consumption factors: A literature review and future research agenda. In World Construction Conference 2012—Global Challenges in Construction Industry; University of Moratuwa: Colombo, Sri Lanka, 2012. [Google Scholar]
  18. Inambao, A.I.F. Review of Factors Affecting Energy Efficiency in Commercial Buildings. Int. J. Mech. Eng. Technol. 2019, 10, 232–244. [Google Scholar]
  19. Torres, M.G.; Pérez-Lombard, L.; Coronel, J.; Maestre, I.; Yan, D. A review on buildings energy information: Trends, end-uses, fuels and drivers. Energy Rep. 2022, 8, 626–637. [Google Scholar] [CrossRef]
  20. Fathi, A.; El Bakkush, A.; Bondinuba, F.; Harris, D. The Effect of Outdoor Air Temperature on the Thermal Performance of a Residential Building. J. Multidiscip. Eng. Sci. Technol. 2015, 2, 3159–3240. [Google Scholar]
  21. Li, M.; Shi, J.; Guo, J.; Cao, J.; Niu, J.; Xiong, M. Climate Impacts on Extreme Energy Consumption of Different Types of Buildings. PLoS ONE 2015, 10, e0124413. [Google Scholar] [CrossRef]
  22. Díaz-López, C.; Verichev, K.; Holgado-Terriza, J.A.; Zamorano, M. Evolution of climate zones for building in Spain in the face of climate change. Sustain. Cities Soc. 2021, 74, 103223. [Google Scholar] [CrossRef]
  23. Walsh, A.; Cóstola, D.; Labaki, L.C. Comparison of three climatic zoning methodologies for building energy efficiency applications. Energy Build. 2017, 146, 111–121. [Google Scholar] [CrossRef] [Green Version]
  24. Walsh, A.; Cóstola, D.; Labaki, L.C. Review of methods for climatic zoning for building energy efficiency programs. Build. Environ. 2017, 112, 337–350. [Google Scholar] [CrossRef] [Green Version]
  25. Walsh, A.; Cóstola, D.; Labaki, L.C. Performance-based validation of climatic zoning for building energy efficiency applications. Appl. Energy 2018, 212, 416–427. [Google Scholar] [CrossRef] [Green Version]
  26. Butera, F.; Aste, N.; Adhikari, R. Sustainable Building Design for Tropical Climates; United Nations Human Settlements Programme (UN-Habitat): Nairobi, Kenya, 2015. [Google Scholar]
  27. Xiong, J.; Yao, R.; Grimmond, S.; Zhang, Q.; Li, B. A hierarchical climatic zoning method for energy efficient building design applied in the region with diverse climate characteristics. Energy Build. 2019, 186, 355–367. [Google Scholar] [CrossRef]
  28. Wang, R.; Lu, S.; Feng, W.; Zhai, X.; Li, X. Sustainable framework for buildings in cold regions of China considering life cycle cost and environmental impact as well as thermal comfort. Energy Rep. 2020, 6, 3036–3050. [Google Scholar] [CrossRef]
  29. Rahman, M. Impact of Climatic Zones of Bangladesh on Office Building Energy Performance. J. Build. Sustain. 2018, 1, 55–63. [Google Scholar]
  30. Albogami, S.; Boukhanouf, R. Residential building energy performance evaluation for different climate zones. IOP Conf. Ser. Earth Environ. Sci. 2019, 329, 012026. [Google Scholar] [CrossRef]
  31. Chen, X.; Yang, H. Integrated energy performance optimization of a passively designed high-rise residential building in different climatic zones of China. Appl. Energy 2018, 215, 145–158. [Google Scholar] [CrossRef]
  32. Walsh, A.; Cóstola, D.; Labaki, L.C. Validation of the climatic zoning defined by ASHRAE standard 169-2013. Energy Policy 2019, 135, 111016. [Google Scholar] [CrossRef]
  33. Khambadkone, N.K.; Jain, R. A bioclimatic analysis tool for investigation of the potential of passive cooling and heating strategies in a composite Indian climate. Build. Environ. 2017, 123, 469–493. [Google Scholar] [CrossRef]
  34. Wang, R.; Lu, S. A novel method of building climate subdivision oriented by reducing building energy demand. Energy Build. 2020, 216, 109999. [Google Scholar] [CrossRef]
  35. Bai, L.; Yang, L.; Song, B.; Liu, N. A new approach to develop a climate classification for building energy efficiency addressing Chinese climate characteristics. Energy 2020, 195, 116982. [Google Scholar] [CrossRef]
  36. López-Ochoa, L.M.; Las-Heras-Casas, J.; López-González, L.M.; Olasolo-Alonso, P. Environmental and energy impact of the EPBD in residential buildings in hot and temperate Mediterranean zones: The case of Spain. Energy 2018, 161, 618–634. [Google Scholar] [CrossRef]
  37. Yang, Y.; Javanroodi, K.; Nik, V.M. Climate change and energy performance of European residential building stocks—A comprehensive impact assessment using climate big data from the coordinated regional climate downscaling experiment. Appl. Energy 2021, 298, 117246. [Google Scholar] [CrossRef]
  38. William, M.A.; Suárez-López, M.J.; Soutullo, S.; Fouad, M.M.; Hanafy, A.A. Enviro-economic assessment of buildings decarbonization scenarios in hot climates: Mindset toward energy-efficiency. Energy Rep. 2022, 8, 172–181. [Google Scholar] [CrossRef]
  39. Benevides, M.N.; Teixeira, D.B.D.S.; Carlo, J.C. Climatic zoning for energy efficiency applications in buildings based on multivariate statistics: The case of the Brazilian semiarid region. Front. Archit. Res. 2022, 11, 161–177. [Google Scholar] [CrossRef]
  40. Bienvenido-Huertas, D.; Marín-García, D.; Carretero-Ayuso, M.J.; Rodríguez-Jiménez, C.E. Climate classification for new and restored buildings in Andalusia: Analysing the current regulation and a new approach based on k-means. J. Build. Eng. 2021, 43, 102829. [Google Scholar] [CrossRef]
  41. Carpio, M.; Jódar, J.; Rodíguez, M.L.; Zamorano, M. A proposed method based on approximation and interpolation for determining climatic zones and its effect on energy demand and CO2 emissions from buildings. Energy Build. 2015, 87, 253–264. [Google Scholar] [CrossRef]
  42. Cory, S.; Lenoir, A.; Donn, M.; Garde, F. Formulating a building climate classification method. In Proceedings of the 12th Conference of International Building Performance Simulation Association Building Simulation 2011, BS 2011, Sydney, NSW, Australia, 14–16 November 2011; pp. 1662–1669. [Google Scholar]
  43. de la Flor, F.J.S.; Domínguez, S.A.; Félix, J.L.M.; Falcón, R.G. Climatic zoning and its application to Spanish building energy performance regulations. Energy Build. 2008, 40, 1984–1990. [Google Scholar] [CrossRef]
  44. Deng, X.; Tan, Z.; Tan, M.; Chen, W. A clustering-based climatic zoning method for office buildings in China. J. Build. Eng. 2021, 42, 102778. [Google Scholar] [CrossRef]
  45. Jain, K.; Gupta, G.; Verma, K.K.; Agarwal, A. Climatic Classification of India for Building Design Using Data Analytics. Natl. Acad. Sci. Lett. 2022, 45, 235–239. [Google Scholar] [CrossRef]
  46. Mazzaferro, L.; Machado, R.M.S.; Melo, A.P.; Lamberts, R. Do we need building performance data to propose a climatic zoning for building energy efficiency regulations? Energy Build. 2020, 225, 110303. [Google Scholar] [CrossRef]
  47. Moral, F.J.; Pulido, E.; Ruíz, A.; López, F. Climatic zoning for the calculation of the thermal demand of buildings in Extremadura (Spain). Theor. Appl. Climatol. 2017, 129, 881–889. [Google Scholar] [CrossRef]
  48. Kishore, K.N.; Rekha, J. A bioclimatic approach to develop spatial zoning maps for comfort, passive heating and cooling strategies within a composite zone of India. Build. Environ. 2018, 128, 190–215. [Google Scholar] [CrossRef]
  49. Roshan, G.; Farrokhzad, M.; Attia, S. Climatic clustering analysis for novel atlas mapping and bioclimatic design recommendations. Indoor Built Environ. 2021, 30, 313–333. [Google Scholar] [CrossRef]
  50. Tükel, M.; Tunçbilek, E.; Komerska, A.; Keskin, G.A.; Arıcı, M. Reclassification of climatic zones for building thermal regulations based on thermoeconomic analysis: A case study of Turkey. Energy Build. 2021, 246, 111121. [Google Scholar] [CrossRef]
  51. Verichev, K.; Zamorano, M.; Carpio, M. Effects of climate change on variations in climatic zones and heating energy consumption of residential buildings in the southern Chile. Energy Build. 2020, 215, 109874. [Google Scholar] [CrossRef]
  52. Yang, L.; Lyu, K.; Li, H.; Liu, Y. Building climate zoning in China using supervised classification-based machine learning. Build. Environ. 2020, 171, 106663. [Google Scholar] [CrossRef]
  53. Zeleke, B.; Kumar, M.; Rajasekar, E. A Novel Building Performance Based Climate Zoning for Ethiopia. Front. Sustain. Cities 2022, 4, 3. [Google Scholar] [CrossRef]
  54. Andric, I.; Al-Ghamdi, S.G. Climate change implications for environmental performance of residential building energy use: The case of Qatar. Energy Rep. 2020, 6, 587–592. [Google Scholar] [CrossRef]
  55. Awadh, O. Sustainability and green building rating systems: LEED, BREEAM, GSAS and Estidama critical analysis. J. Build. Eng. 2017, 11, 25–29. [Google Scholar] [CrossRef]
  56. Rezaallah, A.; Bolognesi, C.; Khoraskani, R.A. LEED and BREEAM; Comparison between policies, assessment criteria and calculation methods. In Proceedings of the 1st International Conference on Building Sustainability Assessment (BSA 2012), Porto, Portugal, 23–25 May 2012. [Google Scholar]
  57. Sanderson, M. The Classification of Climates from Pythagoras to Koeppen. Bull. Am. Meteorol. Soc. 1999, 80, 669–673. [Google Scholar] [CrossRef]
  58. Oliver, J. The history, status and future of climatic classification. Phys. Geogr. 2013, 12, 231–251. [Google Scholar] [CrossRef]
  59. Robinson, A.H.; Wallis, H.M. Humboldt’s Map of Isothermal Lines: A Milestone in Thematic Cartography. Cartogr. J. 1967, 4, 119–123. [Google Scholar] [CrossRef]
  60. Construction Committee of the Russian Soviet Federative Socialist Republic. Rules and Regulations for the Development of Populated Areas, Design and Construction of Buildings and Structures; State Technical Publishing House: Moscow, Russia, 1930.
  61. National Building Code: 1941; National Research Council of Canada: Ottawa, ON, Canada, 1941.
  62. American Society of Heating, Engineers. ASHRAE Standard 90-75: Energy Conservation in New Building Design; American Society of Heating, Refrigerating, and Air-Conditioning Engineers, Incorporated. 1975. Available online: https://www.ojp.gov/ncjrs/virtual-library/abstracts/energy-conservation-new-building-design-impact-assessment-ashrae (accessed on 20 July 2022).
  63. Laustsen, J. Energy Efficiency Requirements in Building Codes: Policies for New Buildings; International Energy Agency (IEA): Paris, France, 2008. [Google Scholar]
  64. Moral-Munoz, J.A.; López-Herrera, A.G.; Herrera-Viedma, E.; Cobo, M.J. Science Mapping Analysis Software Tools: A Review. In Springer Handbook of Science and Technology Indicators; Glänzel, W., Moed, H.F., Schmoch, U., Thelwall, M., Eds.; Springer International Publishing: Cham, Switzerland, 2019; pp. 159–185. [Google Scholar]
  65. Small, H.G. Co-citation in the scientific literature: A new measure of the relationship between two documents. J. Am. Soc. Inf. Sci. 1973, 24, 265–269. [Google Scholar] [CrossRef]
  66. Kessler, M.M. Bibliographic coupling between scientific papers. Am. Doc. 1963, 14, 10–25. [Google Scholar] [CrossRef]
  67. Glänzel, W. National characteristics in international scientific co-authorship relations. Scientometrics 2001, 51, 69–115. [Google Scholar] [CrossRef]
  68. van Eck, N.J.; Waltman, L. Visualizing Bibliometric Networks. In Measuring Scholarly Impact: Methods and Practice; Ding, Y., Rousseau, R., Wolfram, D., Eds.; Springer International Publishing: Cham, Switzerland, 2014; pp. 285–320. [Google Scholar]
  69. Selek, B.; Tuncok, I.K.; Selek, Z. Changes in climate zones across Turkey. J. Water Clim. Chang. 2018, 9, 178–195. [Google Scholar] [CrossRef]
  70. van Eck, N.J.; Waltman, L.R. VOS Viewer: A Computer Program for Bibliometric Mapping; Research Paper, 01/01; Erasmus Research Institute of Management (ERIM), ERIM Is the Joint Research Institute of the Rotterdam School of Management; Erasmus University and the Erasmus School of Economics (ESE) at Erasmus Uni: Rotterdam, The Netherlands, 2009. [Google Scholar]
  71. Shi, J.; Yang, L. A climate classification of China through k-nearest-neighbor and sparse subspace representation. J. Clim. 2020, 33, 243–262. [Google Scholar] [CrossRef]
  72. Zscheischler, J.; Mahecha, M.D.; Harmeling, S. Climate classifications: The value of unsupervised clustering. In Proceedings of the 12th Annual International Conference on Computational Science, ICCS 2012, Omaha, NB, USA, 4–6 June 2012; pp. 897–906. [Google Scholar]
  73. Sarricolea, P.; Herrera-Ossandon, M.; Meseguer-Ruiz, Ó. Climatic regionalisation of continental Chile. J. Maps 2017, 13, 66–73. [Google Scholar] [CrossRef] [Green Version]
  74. Praene, J.P.; Malet-Damour, B.; Radanielina, M.H.; Fontaine, L.; Rivière, G. GIS-based approach to identify climatic zoning: A hierarchical clustering on principal component analysis. Build. Environ. 2019, 164, 106330. [Google Scholar] [CrossRef] [Green Version]
  75. Netzel, P.; Stepinski, T. On using a clustering approach for global climate classification. J. Clim. 2016, 29, 3387–3401. [Google Scholar] [CrossRef]
  76. Mahmoud, A.H.A. An analysis of bioclimatic zones and implications for design of outdoor built environments in Egypt. Build. Environ. 2011, 46, 605–620. [Google Scholar] [CrossRef]
  77. Beck, H.E.; Zimmermann, N.E.; McVicar, T.R.; Vergopolan, N.; Berg, A.; Wood, E.F. Present and future köppen-geiger climate classification maps at 1-km resolution. Sci. Data 2018, 5, 180214 . [Google Scholar] [CrossRef] [Green Version]
  78. Kottek, M.; Grieser, J.; Beck, C.; Rudolf, B.; Rubel, F. World Map of the Köppen-Geiger Climate Classification Updated. Meteorol. Z. 2006, 15, 259–263. [Google Scholar] [CrossRef]
  79. D’Amico, A.; Ciulla, G.; Panno, D.; Ferrari, S. Building energy demand assessment through heating degree days: The importance of a climatic dataset. Appl. Energy 2019, 242, 1285–1306. [Google Scholar] [CrossRef]
  80. Roshan, G.R.; Farrokhzad, M.; Attia, S. Defining thermal comfort boundaries for heating and cooling demand estimation in Iran’s urban settlements. Build. Environ. 2017, 121, 168–189. [Google Scholar] [CrossRef] [Green Version]
  81. Tsikaloudaki, K.; Laskos, K.; Bikas, D. On the establishment of climatic zones in Europe with regard to the energy performance of buildings. Energies 2012, 5, 32–44. [Google Scholar] [CrossRef]
  82. Rakoto-Joseph, O.; Garde, F.; David, M.; Adelard, L.; Randriamanantany, Z.A. Development of climatic zones and passive solar design in Madagascar. Energy Convers. Manag. 2009, 50, 1004–1010. [Google Scholar] [CrossRef]
  83. Verichev, K.; Zamorano, M.; Carpio, M. Assessing the applicability of various climatic zoning methods for building construction: Case study from the extreme southern part of Chile. Build. Environ. 2019, 160, 106165. [Google Scholar] [CrossRef]
  84. Wan, K.K.W.; Li, D.H.W.; Yang, L.; Lama, J.C. Climate classifications and building energy use implications in China. Energy Build. 2010, 42, 1463–1471. [Google Scholar] [CrossRef]
  85. Pusat, S.; Ekmekci, I. A study on degree-day regions of Turkey. Energy Effic. 2016, 9, 525–532. [Google Scholar] [CrossRef]
  86. Bawaneh, K.; Overcash, M.; Twomey, J. Climate zones and the influence on industrial nonprocess energy consumption. J. Renew. Sustain. Energy 2011, 3, 063113. [Google Scholar] [CrossRef]
  87. Lau, C.C.S.; Lam, J.C.; Yang, L. Climate classification and passive solar design implications in China. Energy Convers. Manag. 2007, 48, 2006–2015. [Google Scholar] [CrossRef]
  88. Khedari, J.; Sangprajak, A.; Hirunlabh, J. Thailand climatic zones. Renew. Energy 2002, 25, 267–280. [Google Scholar] [CrossRef]
  89. Wang, H.; Chen, Q. Impact of climate change heating and cooling energy use in buildings in the United States. Energy Build. 2014, 82, 428–436. [Google Scholar] [CrossRef] [Green Version]
  90. Verichev, K.; Salimova, A.; Carpio, M. Thermal and climatic zoning for construction in the southern part of Chile. Adv. Sci. Res. 2018, 15, 63–69. [Google Scholar] [CrossRef] [Green Version]
  91. Singh, M.K.; Mahapatra, S.; Atreya, S.K. Development of bio-climatic zones in north-east India. Energy Build. 2007, 39, 1250–1257. [Google Scholar] [CrossRef]
  92. Lamberts, R.; Roriz, M.; Ghisi, E. Bioclimatic zoning of Brazil: A proposal based on the givoni and mohoney methods. In Proceedings of the Sustaining the Future: Energy, Ecology, Architecture: Plea ′99—The 16th International Conference Plea (Passive & Low Energy Architecture), Brisbane, Australia, 22–24 September 1999. [Google Scholar]
  93. Erell, E.; Portnov, B.; Etzion, Y. Mapping the potential for climate-conscious design of buildings. Build. Environ. 2003, 38, 271–281. [Google Scholar] [CrossRef]
  94. Unal, Y.; Kindap, T.; Karaca, M. Redefining the climate zones of Turkey using cluster analysis. Int. J. Climatol. 2003, 23, 1045–1055. [Google Scholar] [CrossRef]
  95. Fovell, R.G.; Fovell, M.Y.C. Climate zones of the conterminous United States defined using cluster analysis. J. Clim. 1993, 6, 2103–2135. [Google Scholar] [CrossRef]
  96. Alrashed, F.; Asif, M. Climatic Classifications of Saudi Arabia for Building Energy Modelling. In Proceedings of the 7th International Conference on Applied Energy, ICAE 2015, Abu Dhabi, United Arab Emirates, 28–31 March 2015; pp. 1425–1430. [Google Scholar]
  97. Falquina, R.; Gallardo, C. Development and application of a technique for projecting novel and disappearing climates using cluster analysis. Atmos. Res. 2017, 197, 224–231. [Google Scholar] [CrossRef]
  98. Chen, Y.; Li, M.; Cao, J.; Cheng, S.; Zhang, R. Effect of climate zone change on energy consumption of office and residential buildings in China. Theor. Appl. Climatol. 2021, 144, 353–361. [Google Scholar] [CrossRef]
  99. Pernigotto, G.; Gasparella, A. Classification of European Climates for Building Energy Simulation Analyses. In Proceedings of the International Conference on High Performance, Tokyo, Japan, 28–31 January 2018. [Google Scholar]
  100. Pernigotto, G.; Walsh, A.; Gasparella, A.; Hensen, J.L.M. Clustering of European climates and representative climate identification for building energy simulation analyses. In Proceedings of the 16th International Conference of the International Building Performance Simulation Association, Building Simulation, Rome, Italy, 2–4 September 2019; Volume 2019, pp. 4833–4840. [Google Scholar]
  101. Aparecido, L.E.O.; Rolim, G.S.; Richetti, J.; de Souza, P.S.; Johann, J.A. Köppen, Thornthwaite and Camargo climate classifications for climatic zoning in the State of Paraná, Brazil. Cienc. Agrotecnol. 2016, 40, 405–417. [Google Scholar] [CrossRef] [Green Version]
  102. Peel, M.C.; Finlayson, B.L.; McMahon, T.A. Updated world map of the Köppen-Geiger climate classification. Hydrol. Earth Syst. Sci. 2007, 11, 1633–1644. [Google Scholar] [CrossRef] [Green Version]
  103. Ascencio-Vásquez, J.; Brecl, K.; Topič, M. Methodology of Köppen-Geiger-Photovoltaic climate classification and implications to worldwide mapping of PV system performance. Sol. Energy 2019, 191, 672–685. [Google Scholar] [CrossRef]
  104. Bai, L.; Wang, S. Definition of new thermal climate zones for building energy efficiency response to the climate change during the past decades in China. Energy 2019, 170, 709–719. [Google Scholar] [CrossRef]
  105. van Schijndel, A.W.M.; Schellen, H.L. The simulation and mapping of building performance indicators based on European weather stations. Front. Archit. Res. 2013, 2, 121–133. [Google Scholar] [CrossRef] [Green Version]
  106. Semahi, S.; Benbouras, M.A.; Mahar, W.A.; Zemmouri, N.; Attia, S. Development of spatial distribution maps for energy demand and thermal comfort estimation in Algeria. Sustainability 2020, 12, 6066. [Google Scholar] [CrossRef]
  107. Mazzaferro, L.; Machado, R.M.S.; Melo, A.P.; Lamberts, R. Climatic zoning methodology based on data-driven approach. In Proceedings of the 16th International Conference of the International Building Performance Simulation Association, Building Simulation, Rome, Italy, 2–4 September 2019; Volume 2019, pp. 3955–3962. [Google Scholar]
  108. De Rosa, M.; Bianco, V.; Scarpa, F.; Tagliafico, L.A. Historical trends and current state of heating and cooling degree days in Italy. Energy Convers. Manag. 2015, 90, 323–335. [Google Scholar] [CrossRef]
  109. Díaz-López, C.; Jódar, J.; Verichev, K.; Rodríguez, M.L.; Carpio, M.; Zamorano, M. Dynamics of changes in climate zones and building energy demand. A case study in Spain. Appl. Sci. 2021, 11, 4261. [Google Scholar] [CrossRef]
  110. Ghedamsi, R.; Settou, N.; Gouareh, A.; Khamouli, A.; Saifi, N.; Recioui, B.; Dokkar, B. Modeling and forecasting energy consumption for residential buildings in Algeria using bottom-up approach. Energy Build. 2016, 121, 309–317. [Google Scholar] [CrossRef]
  111. Danilovich, I.; Geyer, B. Estimates of current and future climate change in Belarus based on meteorological station data and the EURO-CORDEX-11 dataset. Meteorol. Hydrol. Water Manag. 2021, 9. [Google Scholar] [CrossRef]
  112. Vondráková, A.; Vávra, A.; Voženílek, V. Climatic regions of the Czech Republic. J. Maps 2013, 9, 425–430. [Google Scholar] [CrossRef] [Green Version]
  113. da Casa Martín, F.; Valiente, E.E.; Celis, D.F. Climate zoning for its application to bioclimatic design. Application in Galicia (Spain). Inf. Constr. 2017, 69. [Google Scholar] [CrossRef] [Green Version]
  114. Muddu, R.D.; Gowda, D.M.; Robinson, A.J.; Byrne, A. Optimisation of retrofit wall insulation: An Irish case study. Energy Build. 2021, 235, 110720. [Google Scholar] [CrossRef]
  115. Noh, B.; Choi, J.; Seo, D. A Study on the Classification Criteria of Climatic Zones in Korean Building Code Based on Heating Degree-Days. Korean J. Air-Cond. Refrig. Eng. 2015, 27, 574–580. [Google Scholar]
  116. Ogunsote, O.; Prucnal-Ogunsote, B. Defining climatic zones for architectural design in Nigeria: A systematic delineation. J. Environ. Technol. 2002, 1, 1–14. [Google Scholar]
  117. Mobolade, T.D.; Pourvahidi, P. Bioclimatic approach for climate classification of Nigeria. Sustainability 2020, 12, 4192. [Google Scholar] [CrossRef]
  118. Hobaica, M.; Allard, F.; Belarbi, R. Passive Cooling Systems for Buildings. Potential of Use within Venezuela’s Climatic Zones. Available online: https://hal.science/hal-00312480/ (accessed on 5 May 2022).
  119. Malmgren, B.A.; Winter, A. Climate zonation in Puerto Rico based on principal components analysis and an artificial neural network. J. Clim. 1999, 12, 977–985. [Google Scholar] [CrossRef]
  120. Izzo, M.; Rosskopf, C.M.; Aucelli, P.P.; Maratea, A.; Méndez, R.; Pérez, C.; Segura, H. A new climatic map of the dominican republic based on the thornthwaite classification. Phys. Geogr. 2010, 31, 455–472. [Google Scholar] [CrossRef]
  121. Felix, L.D.P.J.; Izquierdo, R. Análisis comparativo de las diferentes zonas climáticas de la república dominicana. In Proceedings of the 1st Iberic Conference on Theoretical and Experimental Mechanics and Materials/11th National Congress on Experimental Mechanics, Porto, Portugal, 4–7 November 2018; pp. 865–876. [Google Scholar]
  122. Verichev, K.; Carpio, M. Climatic zoning for building construction in a temperate climate of Chile. Sustain. Cities Soc. 2018, 40, 352–364. [Google Scholar] [CrossRef]
  123. Hjortling, C.; Björk, F.; Berg, M.; Klintberg, T.A. Energy mapping of existing building stock in Sweden—Analysis of data from Energy Performance Certificates. Energy Build. 2017, 153, 341–355. [Google Scholar] [CrossRef]
  124. Kunchornrat, A.; Namprakai, P.; Pont, P.T. The impacts of climate zones on the energy performance of existing Thai buildings. Resour. Conserv. Recycl. 2009, 53, 545–551. [Google Scholar] [CrossRef]
  125. Gangolells, M.; Casals, M.; Forcada, N.; MacArulla, M.; Cuerva, E. Energy mapping of existing building stock in Spain. J. Clean. Prod. 2016, 112, 3895–3904. [Google Scholar] [CrossRef]
  126. Dena, A.J.G.; Pascual, M.Á.; Bandera, C.F. Building energy model for mexican energy standard verification using physics-based open studio sgsave software simulation. Sustainability 2021, 13, 1521. [Google Scholar] [CrossRef]
  127. Elmzughi, M.; Alghoul, S.; Mashena, M. Optimizing thermal insulation of external building walls in different climate zones in Libya. J. Build. Phys. 2021, 45, 368–390. [Google Scholar] [CrossRef]
  128. Coskun, C.; Ertürk, M.; Oktay, Z.; Hepbasli, A. A new approach to determine the outdoor temperature distributions for building energy calculations. Energy Convers. Manag. 2014, 78, 165–172. [Google Scholar] [CrossRef]
  129. Bodach, S. Developing bioclimatic zones and passive solar design strategies for Nepal. In Proceedings of the 30th International PLEA Conference: Sustainable Habitat for Developing Societies: Choosing the Way Forward—Proceedings, Ahmedabad, India, 16–18 December 2014; pp. 167–174. [Google Scholar]
  130. Kim, Y.; Jang, H.K.; Yu, K.H. Study on extension of standard meteorological data for cities in South Korea Using ISO 15927-4. Atmosphere 2017, 8, 220. [Google Scholar] [CrossRef] [Green Version]
  131. Moradchelleh, A. Construction design zoning of the territory of Iran and climatic modeling of civil buildings space. J. King Saud Univ.—Sci. 2011, 23, 355–369. [Google Scholar] [CrossRef]
  132. Aliaga, V.S.; Ferrelli, F.; Piccolo, M.C. Regionalization of climate over the Argentine Pampas. Int. J. Climatol. 2017, 37, 1237–1247. [Google Scholar] [CrossRef]
  133. Pineda-Martínez, L.F.; Carbajal, N.; Medina-Roldán, E. Regionalization and classification of bioclimatic zones in the central-northeastern region of México using principal component analysis (PCA). Atmosfera 2007, 20, 133–145. [Google Scholar]
  134. Bhatnagar, M.; Mathur, J.; Garg, V. Climate zone classification of India using new base temperature. In Proceedings of the 16th International Conference of the International Building Performance Simulation Association, Building Simulation 2019, Rome, Italy, 2–4 September 2019; pp. 4841–4845. [Google Scholar]
  135. Pawar, A.S.; Mukherjee, M.; Shankar, R. Thermal comfort design zone delineation for India using GIS. Build. Environ. 2015, 87, 193–206. [Google Scholar] [CrossRef]
  136. Nair, R.J.; Brembilla, E.; Hopfe, C.; Mardaljevic, J. Weather data for building simulation: Grid resolution for climate zone delineation. In Proceedings of the 16th International Conference of the International Building Performance Simulation Association, Building Simulation 2019, Rome, Italy, 2–4 September 2019; pp. 3932–3939. [Google Scholar]
  137. Jittawikul, A.; Saito, I.; Ishihara, O. Climatic Maps for Passive Cooling Methods Utilization in Thailand. J. Asian Archit. Build. Eng. 2004, 3, 109–114. [Google Scholar] [CrossRef] [Green Version]
  138. Anas, H.; El Mghouchi, Y.; Halima, Y.; Nawal, A.; Mohamed, C. Novel climate classification based on the information of solar radiation intensity: An application to the climatic zoning of Morocco. Energy Convers. Manag. 2021, 247, 114770. [Google Scholar] [CrossRef]
  139. Briggs, R.S.; Lucas, R.G.; Taylor, Z.T. Climate classification for building energy codes and standards: Part 1—Development process. In Technical and Symposium Papers Presented At the 2003 Winter Meeting of The ASHRAE; ASHRAE Transactions: Chicago, IL, USA, 2003; pp. 109–121. [Google Scholar]
  140. Briggs, R.S.; Lucas, R.G.; Taylor, Z.T. Climate classification for building energy codes and standards: Part 2—Zone definitions, maps, and comparisons. In Technical and Symposium Papers Presented At the 2003 Winter Meeting of The ASHRAE; ASHRAE Transactions: Chicago, IL, USA, 2003; pp. 122–130. [Google Scholar]
  141. Abebe, S.; Assefa, T. Development of climatic zoning and energy demand prediction for Ethiopian cities in degree days. Energy Build. 2022, 260, 111935. [Google Scholar] [CrossRef]
  142. Lam, J.C.; Yang, L.; Liu, J. Development of passive design zones in China using bioclimatic approach. Energy Convers. Manag. 2006, 47, 746–762. [Google Scholar] [CrossRef]
  143. Butera, F.M. Sustainable Building Design for Tropical Climates. Principles and Applications for Eastern Africa; Nairobi United Nations Human Settlements Programme (UN-Habitat): Nairobi, Kenya, 2014. [Google Scholar]
  144. Ferstl, K. Climate and Human Settlements—Integrating Climate into Urban Planning and Building Design in Africa; UNEP: Nairobi, Kenya, 1991. [Google Scholar]
  145. Poulsen, M.; Lauring, M.; Brunsgaard, C. A review of climate change adaptive measures in architecture within temperate climate zones. J. Green Build. 2020, 15, 113–130. [Google Scholar] [CrossRef]
  146. Navarro, F.C. Arquitetura e Clima na Bolívia: Uma Proposta de Zoneamento Bioclimático. Ph.D. Thesis, Universidade Estadual de Campinas Faculdade de Engenharia Civil, Arquitetura e Urbanismo, Campinas, Spain, 2007. [Google Scholar] [CrossRef]
  147. Asfaw, S.A. Developing Parametric Solar Envelope for Ethiopian Cities; School of Graduate Studies of Addis Ababa University in Partial Fulfillment of the Requirements of the Masters of Science in Urban Design and Development, Ethiopia Institute of Architecture Building Construction and City Development: Addis Ababa, Ethiopia, 2020. [Google Scholar]
  148. Arens, E.A.; Williams, P.B. The effect of wind on energy consumption in buildings. Energy Build. 1977, 1, 77–84. [Google Scholar] [CrossRef]
  149. Diaz, C.A.; Osmond, P. Influence of Rainfall on the Thermal and Energy Performance of a Low Rise Building in Diverse Locations of the Hot Humid Tropics. Procedia Eng. 2017, 180, 393–402. [Google Scholar] [CrossRef]
  150. Jovanović, S.; Savić, S.; Bojić, M.; Djordjević, Z.; Nikolić, D. The impact of the mean daily air temperature change on electricity consumption. Energy 2015, 88, 604–609. [Google Scholar] [CrossRef]
  151. Ministry of Environment and Sustainable Development Vice Ministry of Environment and Sustainable Development Directorate of Environmental. Environmental Criteria for the Design and Construction of Urban Housing; Ministerio de Ambiente y Desarrollo Sostenible: Bogotá, Colombia, 2012.
  152. Corporal-Lodangco, I.L.; Leslie, L.M. Defining Philippine Climate Zones Using Surface and High-Resolution Satellite Data. Procedia Comput. Sci. 2017, 114, 324–332. [Google Scholar] [CrossRef]
  153. Meng, F.; Li, M.; Cao, J.; Li, J.; Xiong, M.; Feng, X.; Ren, G. The effects of climate change on heating energy consumption of office buildings in different climate zones in China. Theor. Appl. Climatol. 2017, 133, 521–530. [Google Scholar] [CrossRef]
  154. Bodach, S.; Lang, W.; Auer, T. Design guidelines for energy-efficient hotels in Nepal. Int. J. Sustain. Built Environ. 2016, 5, 411–434. [Google Scholar] [CrossRef] [Green Version]
  155. Dowd, P.; Wang, H.; Pardo-Iguzquiza, E.; Yongguo, Y. Constrained Spatial Clustering of Climate Variables for Geostatistical Reconstruction of Optimal Time Series and Spatial Fields. In Geostatistics Valencia 2016; Springer: Berlin/Heidelberg, Germany, 2017; pp. 879–891. [Google Scholar]
  156. Daly, C. Guidelines for assessing the stability of spatial climate data sets. Int. J. Climatol. 2006, 26, 707–721. [Google Scholar] [CrossRef]
  157. Raymundo, C.E.; Oliveira, M.C.; Eleuterio, T.D.A.; André, S.R.; da Silva, M.G.; Queiroz, E.R.D.S.; Medronho, R.D.A. Spatial analysis of COVID-19 incidence and the sociodemographic context in Brazil. PLoS ONE 2021, 16, e0247794. [Google Scholar] [CrossRef] [PubMed]
  158. Hall, A.; Jones, G.V. Spatial analysis of climate in winegrape-growing regions in Australia. Aust. J. Grape Wine Res. 2010, 16, 389–404. [Google Scholar] [CrossRef]
  159. Hammer, R.B.; Stewart, S.I.; Winkler, R.L.; Radeloff, V.C.; Voss, P.R. Characterizing dynamic spatial and temporal residential density patterns from 1940–1990 across the North Central United States. Landsc. Urban Plan. 2004, 69, 183–199. [Google Scholar] [CrossRef]
  160. Tobler, W. On the first law of geography: A reply. Ann. Assoc. Am. Geogr. 2004, 94, 304–310. [Google Scholar] [CrossRef]
  161. Anselin, L. Local Indicators of Spatial Association—LISA. Ann. Assoc. Am. Geogr. 1995, 27, 93–115. [Google Scholar] [CrossRef]
  162. Day, T. TM 41 Degree-days: Theory and application. In TM 41 Degree-Days: Theory and Application; Chartered Institution of Building Services Engineers (CIBSE): London, UK, 2006. [Google Scholar]
  163. ANSI/ASHRAE Standard 169-2021; Climatic Data for Building Design Standards. American Society of Heating, Refrigerating and Air-Conditioning Engineers: Atlanta, GA, USA, 2021.
  164. Guttman, N.B.; Lehman, R.L. Estimation of Daily Degree-hours. J. Appl. Meteorol. 1992, 31, 797. [Google Scholar] [CrossRef]
  165. Hitchin, E.R. Estimating monthly degree-days. Build. Serv. Eng. Res. Technol. 1983, 4, 159–162. [Google Scholar] [CrossRef]
  166. Schoenau, G.; Kehrig, R.A. Method for calculating degree-days to any base temperature. Energy Build. 1990, 14, 299–302. [Google Scholar] [CrossRef]
  167. Omarov, B.; Memon, S.A.; Kim, J. A novel approach to develop climate classification based on degree days and building energy performance. Energy 2023, 267, 126514. [Google Scholar] [CrossRef]
  168. Quayle, R.G.; Diaz, H.F. Heating Degree Day Data Applied to Residential Heating Energy Consumption. J. Appl. Meteorol. 1980, 19, 241–246. [Google Scholar] [CrossRef]
  169. Le Comte, D.M.; Warren, H.E. Modeling the Impact of Summer Temperatures on National Electricity Consumption. J. Appl. Meteorol. 1981, 20, 1415–1419. [Google Scholar] [CrossRef]
  170. Lehman, R.L.; Warren, H.E. Residential Natural Gas Consumption: Evidence That Conservation Efforts to Date Have Failed. Science 1978, 199, 879–882. [Google Scholar] [CrossRef] [PubMed]
  171. Warren, H.E.; LeDuc, S.K. Impact of Climate on Energy Sector in Economic Analysis. J. Appl. Meteorol. 1981, 20, 1431–1439. [Google Scholar] [CrossRef]
  172. Strahler, A.N. Physical Geography; John Willey: New York, NY, USA, 1969. [Google Scholar]
  173. Bhatnagar, M.; Mathur, J.; Garg, V. Determining base temperature for heating and cooling degree-days for India. J. Build. Eng. 2018, 18, 270–280. [Google Scholar] [CrossRef]
  174. Crawley, D. Building Performance Simulation: A Tool for Policymaking. Ph.D. Thesis, University of Strathclyde, Glasgow, UK, 2008. [Google Scholar]
  175. Dias, J.B.; da Graça, G.C.; Soares, P.M.M. Comparison of methodologies for generation of future weather data for building thermal energy simulation. Energy Build. 2020, 206, 109556. [Google Scholar] [CrossRef]
  176. Tootkaboni, M.P.; Ballarini, I.; Zinzi, M.; Corrado, V. A Comparative Analysis of Different Future Weather Data for Building Energy Performance Simulation. Climate 2021, 9, 37. [Google Scholar] [CrossRef]
  177. Givoni, B. Man, Climate, and Architecture; Elsevier Publishing Company Limited: New York, NY, USA, 1969. [Google Scholar]
  178. Givoni, B. Comfort, climate analysis and building design guidelines. Energy Build. 1992, 18, 11–23. [Google Scholar] [CrossRef]
  179. Milne, B.G.M. Architectural design based on climate. Energy Conserv. Through Build. Des. 1979, 96–113. [Google Scholar]
  180. Olgyay, V. Design with Climate: A Bioclimatic Approach to Architectural Regionalism; Van Nostrand Reinhold: New York, NY, USA, 1992. [Google Scholar]
  181. Pajek, L.; Košir, M. Implications of present and upcoming changes in bioclimatic potential for energy performance of residential buildings. Build. Environ. 2018, 127, 157–172. [Google Scholar] [CrossRef]
  182. Walker, C.L.; Hasanzadeh, S.; Esmaeili, B.; Anderson, M.R.; Dao, B. Developing a winter severity index: A critical review. Cold Reg. Sci. Technol. 2019, 160, 139–149. [Google Scholar] [CrossRef]
  183. Boustead, B.M.; Hilberg, S.; Shulski, M.; Hubbard, K. The Accumulated Winter Season Severity Index (AWSSI). J. Appl. Meteorol. Climatol. 2015, 54, 150326122910004. [Google Scholar] [CrossRef] [Green Version]
  184. Federici, A.; Iatauro, D.; Romeo, C.; Signoretti, P.; Terrinoni, L. Climatic Severity Index: Definition of Summer Climatic Zones in Italy through the Assessment of Air Conditioning Energy Need in Buildings. In Proceedings of the Clima 2013 RHEVA Word Congress & International Conference on IAQVECAt, Prague, Czech Republic, 16–19 June 2013. [Google Scholar]
  185. Koppen, W. Das geographische System der Klimate; Gebrüder Borntraeger: Berlin, Germany, 1936. [Google Scholar]
  186. Humphreys, M. Outdoor temperatures and comfort indoors. Batim. Int. Build. Res. Pract. 1978, 6, 92. [Google Scholar] [CrossRef]
  187. Huang, J.; Ritschard, R.L.; Bull, J.C.; Chang, L. Climatic indicators for estimating residential heating and cooling loads. In ASHRAE Transactions; Lawrence Berkeley Lab.: Berkeley, CA, USA, 1987; pp. 72–111. [Google Scholar]
  188. Eto, J.H. On using degree-days to account for the effects of weather on annual energy use in office buildings. Energy Build. 1988, 12, 113–127. [Google Scholar] [CrossRef]
  189. Kershaw, T.; Eames, M.; Coley, D. Comparison of multi-year and reference year building simulations. Build. Serv. Eng. Res. Technol. 2010, 31, 357–369. [Google Scholar] [CrossRef] [Green Version]
  190. Nguyen, A.T.; Tran, Q.B.; Tran, D.Q.; Reiter, S. An investigation on climate responsive design strategies of vernacular housing in Vietnam. Build. Environ. 2011, 46, 2088–2106. [Google Scholar] [CrossRef] [Green Version]
  191. Rubel, F.; Brugger, K.; Haslinger, K.; Auer, I. The climate of the European Alps: Shift of very high resolution Köppen-Geiger climate zones 1800–2100. Meteorol. Z. 2017, 26, 115–125. [Google Scholar] [CrossRef]
  192. Rubel, F.; Kottek, M. Comments on: "The thermal zones of the Earth by Wladimir Köppen (1884). Meteorol. Z. 2011, 20, 361–365. [Google Scholar] [CrossRef]
  193. Rubel, F.; Kottek, M. Observed and projected climate shifts 1901–2100 depicted by world maps of the Köppen-Geiger climate classification. Meteorol. Z. 2010, 19, 135–141. [Google Scholar] [CrossRef] [Green Version]
  194. Köppen, W.; Volken, E.; Brönnimann, S. The thermal zones of the Earth according to the duration of hot, moderate and cold periods and to the impact of heat on the organic world. Meteorol. Z. 2011, 20, 351–360. [Google Scholar] [CrossRef] [PubMed]
  195. Santamouris, M. Energy and Climate in the Urban Built Environment; Routledge: Oxfordshire, UK, 2013. [Google Scholar]
  196. Santamouris, M.; Papanikolaou, N.; Livada, I.; Koronakis, I.; Georgakis, C.; Argiriou, A.; Assimakopoulos, D.N. On the impact of urban climate on the energy consumption of building. Solar Energy 2001, 70, 201–216. [Google Scholar] [CrossRef]
  197. Attia, S. Net Zero Energy Buildings (NZEB): Concepts, Frameworks and Roadmap for Project Analysis and Implementation; Butterworth-Heinemann: Oxford, UK, 2018. [Google Scholar]
  198. Attia, S.; Gratia, E.; De Herde, A.; Hensen, J.L.M. Simulation-based decision support tool for early stages of zero-energy building design. Energy Build. 2012, 49, 2–15. [Google Scholar] [CrossRef] [Green Version]
  199. Attia, S.; Hamdy, M.; O’Brien, W.; Carlucci, S. Assessing gaps and needs for integrating building performance optimization tools in net zero energy buildings design. Energy Build. 2013, 60, 110–124. [Google Scholar] [CrossRef] [Green Version]
  200. Givoni, B. Indoor temperature reduction by passive cooling systems. Sol. Energy 2011, 85, 1692–1726. [Google Scholar] [CrossRef]
  201. Attia, S.; Lacombe, T.; Rakotondramiarana, H.T.; Garde, F.; Roshan, G. Analysis tool for bioclimatic design strategies in hot humid climates. Sustain. Cities Soc. 2019, 45, 8–24. [Google Scholar] [CrossRef] [Green Version]
Figure 1. The review methodology flowchart.
Figure 1. The review methodology flowchart.
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Figure 2. Histogram of publication years.
Figure 2. Histogram of publication years.
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Figure 3. The sources of the academic papers (a) and types of documents in the review lists (b).
Figure 3. The sources of the academic papers (a) and types of documents in the review lists (b).
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Figure 4. Main variables for CZB.
Figure 4. Main variables for CZB.
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Figure 5. The number of climate variables used for CZB.
Figure 5. The number of climate variables used for CZB.
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Figure 6. The most popular combinations of two climate variables used for CZB.
Figure 6. The most popular combinations of two climate variables used for CZB.
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Figure 7. The most common climate data sources.
Figure 7. The most common climate data sources.
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Figure 8. The most prevalent forms of climatic data used to develop the classifications.
Figure 8. The most prevalent forms of climatic data used to develop the classifications.
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Figure 9. Histogram of climate observation periods.
Figure 9. Histogram of climate observation periods.
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Figure 10. Histogram of years passed from last observation date to publication.
Figure 10. Histogram of years passed from last observation date to publication.
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Figure 11. Different methods in CZB.
Figure 11. Different methods in CZB.
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Figure 12. Frequency of the number of methods used for CZB.
Figure 12. Frequency of the number of methods used for CZB.
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Figure 13. A map of affiliations or public organizations which publish more articles than others in CZB.
Figure 13. A map of affiliations or public organizations which publish more articles than others in CZB.
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Figure 14. The bar chart of the journals that published CZB papers.
Figure 14. The bar chart of the journals that published CZB papers.
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Figure 15. The bar chart of the most-contributing authors in the CZB area. The number of published CZB papers is shown at the outside end of each bar.
Figure 15. The bar chart of the most-contributing authors in the CZB area. The number of published CZB papers is shown at the outside end of each bar.
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Figure 16. The ratio of citations to the year of publication and papers cited above trend.
Figure 16. The ratio of citations to the year of publication and papers cited above trend.
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Figure 17. Co-citation network of researchers.
Figure 17. Co-citation network of researchers.
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Figure 18. Bibliographic coupling network of authors.
Figure 18. Bibliographic coupling network of authors.
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Figure 19. Direct citation network of articles.
Figure 19. Direct citation network of articles.
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Figure 20. Co-occurrence network of keywords.
Figure 20. Co-occurrence network of keywords.
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Figure 21. Histogram of publications in this review concerning future climate scenarios.
Figure 21. Histogram of publications in this review concerning future climate scenarios.
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Figure 22. Bibliographic coupling of countries.
Figure 22. Bibliographic coupling of countries.
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Table 1. Data collected during the review.
Table 1. Data collected during the review.
NumberReferenceYear of the Source PublicationEntire Territory of or Part of the CountryCountry/RegionMain VariablesNumber of Climate Variables Used for Climate ZoningClimate Data SourceClimate Data Source NameInitial Data FormData Information Observation Period (Years)Methods Used for Climate ZoningNumber of Methods UsedMethods DetailsNumber of Zones Defined
1[9]2020Entire territory of BelgiumDDs1Web databaseAgri4Cast datasetDaily mean values1976–2004 (30)DDM1Base temperatures: HDD 18 °C; CDD 18 °C7
2[27]2019Part ofChina (hot summer and cold winter (HSCW) zone)DDs, RH, SR, W, TMY5National meteorological service National meteorological service Daily mean/maximum/minimum values, Hourly values TMY2006–2015 (10)DDM, MLM, BES3Two-tier classification with hierarchical agglomerative clustering (HAC). EnergyPlus simulations with 1 archetype7
3[23]2017Entire territory of NicaraguaAT, RH, SR, W4SoftwareAutodesk Green Building Studio (GBS)Hourly values DDM, MLM, Administrative division3K-nearest neighbors algorithm3
4[79]2019Entire territory of ItalyDDs, Al, TMY3National meteorological service Italian Military Air Force weather stations.Daily mean values, Hourly values TMY2000–2009 (10)DDM, BES2Base temperatures: HDD 12 °C; CDD 12 °C, TRNSYS simulations with 13 archetypes6
5[80]2017Entire territory of IranAT, RH, DDs3National meteorological service Iran Meteorological OrganizationDaily mean values1995–2014 (20)DDM, BCM2Milne-Givoni chart8
6[81]2012 EuropeDDs1 Monthly mean values DDM, BES2Base temperatures: HDD 18 °C; CDD 18 °C5
7[74]2019Entire territory of MadagascarRH, GHI, Pr3 MLM1Hierarchical k-means clustering on principal components (HCPC)3
8[82]2009Entire territory of MadagascarAT, SR, W3National meteorological service Meteorological forecast utilities of Antananarivo.Monthly mean values(20)BCM1 6
9[25]2018Entire territory of NicaraguaTMY1SoftwareAutodesk Green Building Studio (GBS)Hourly values TMY DDM, MLM, Administrative division, BES4EnergyPlus simulations with 4 archetypes3
10[10]2012Entire territory of IranDDs1 Daily mean values1961–1990 (40)DDM1Base temperatures: HDD 18 °C; CDD 24 °C
11[32]2019Part ofUnited States (States of Florida, Georgia, and Tennessee)TMY1National meteorological service The U.S. Department of Energy (DOE)Hourly values TMY DDM, BES2EnergyPlus simulations with 13 archetypes4
12[83]2019Entire territory of ChileTMY, DDs, SR, Pr, RH, W6SoftwareAutodesk Green Building Studio (GBS) Mesoscale Meteorological Model, Version 5 (MM5)Hourly values TMY2007–2017 (11)DDM, MLM, BCM, BES4Base temperatures: HDD 18 °C; CDD 10 °C5
13[84]2010Entire territory of ChinaAT, RH2Web databaseCRU TS 2.1 data set from the University of East Anglia1224 records of monthly minimum temperature, maximum temperature and vapor pressure, annual cumulative heat and cold stresses1901–2002 (102)MLM, HCI 2Hierarchical
cluster tree of comfort index and heat/cold stresses,
8
14[46]2020Entire territory of BrazilDDs, AT, RH, Pr4National meteorological service INMET databaseHourly values TMY(10)DDM, KGM, BES, enhanced degree-day method, MLM, etc.7Base temperatures: HDD 18 °C; CDD 10 °C8
15[85]2016Entire territory of TurkeyDDs1 Hourly values TMY1989–2009 (20)DDM1Base temperatures: HDD 18 °C; CDD 18 °C4
16[86]2011Entire territory of United StatesDDs1 Daily mean values(5)DDM1 5
17[41]2015Part ofSpain (Andalusia)DDs, SR, AT, Al4National meteorological service Agencia Andaluza de la Energía (Andalusian Energy Agency) CSIM, BES2Approximation and interpolation method (AIM), CERMA software simulations with 1 archetype3
18[87]2007Entire territory of ChinaSR1 Monthly mean values1957–2000 (10–44)MLM1 5
19[88]2002Entire territory of ThailandAT, RH2National meteorological service Meteorological Department of Thailand3 h values1981–1998 (18)FDV2Frequency distribution of occurrence of maximum and minimum values4
20[89]2014Entire territory of United StatesTMY1Research institutionNational Renewable Energy Laboratory.Monthly mean values1991–2005 (15)BES1EnergyPlus simulations with 9 archetypes7
21[43]2008Part ofSpain (Andalusia)DDs, SR, Al3National meteorological service the Andalusian Regional GovernmentMonthly mean values1970–2006 (37)DDM1Al correction and approximation and interpolation method (AIM)12
22[73]2017Entire territory of ChileAT, Pr2Web databaseGlobal Historical Climate Network
Dataset (GHCN), FAOClim 2.0
Annual and monthly mean values1950–2000 (50)KGM1 25
23[90]2018Part ofChile (southern part)DDs, SR2National meteorological service the Ministry of Agriculture of Chile (Agromet), the Ministry of Environment (MMA) and the Di-
rectorate General of Civil Aviation (DGAC)
Hourly values2008–2018 (10)DDM, CSIM2Base temperature: HDD 15 °C5
24[91]2007Part ofIndia (northeast region)AT, RH, Pr, W4National meteorological service Regional Meteorological Centre, Guwahati, IndiaMonthly mean values(30)BCM1Milne, Givoni charts4
25[76]2011Entire territory of EgyptAT, RH2National meteorological service General
Meteorological Authority, Cairo, Egypt
Monthly mean values(30)BCM1ASHRAE charts8
26[47]2016Part ofSpain (Extremadura)DDs, SR, Al3National meteorological service the National Meteorological Agency and the Regional Government of Extremadura.Monthly mean values1976–2011 (10)CSIM1Approximation and interpolation method (AIM)5
27[92]1999Entire territory of BrazilAT, RH2 Monthly mean values BCM1 8
28[93]2003Entire territory of IsraelAT, RH, SR, W4 Daily mean values MLM1Hierarchical clustering7
29[94]2003Entire territory of TurkeyAT, Pr2National meteorological service National Weather Service of TurkeyMonthly mean values1951–1998 (47)MLM1Hierarchical clustering7
30[95]1993Entire territory of United StatesAT, Pr2National meteorological service National climatic data center Monthly mean values1931–1980 (50)MLM1Principal component analysis, hierarchical clustering8, 14, 25
31[48]2018Entire territory of IndiaAT, RH, SR, TMY4National meteorological service Indian Society of Heating Refrigeration and Air-Conditioning Engineers (ISHRAE)Hourly values TMY BCM, BES2Ecotect analysis program simulation with 1 archetype (duplex house)5
32[96] *2015Entire territory of Saudi ArabiaAT, RH, W, SR4National meteorological service MEPA. The Meteorology and Environmental Protection Administration (MEPA) weather tapes in Jeddah, Saudi
Arabia
1960–2010 (20)KGM, TCCM, MLM, The World Health Organization classification method, etc.16 6
33[72] *2012 WorldAT, Pr, SR3Web databaseCRU and GPCC data sets, ERA-Interim, MODISMonthly mean values2001–2007 (8)KGM, MLM2Principal component analysis, k-means clustering12
34[97]2017 WorldAT, Pr2Climate modelGCM ensembleMonthly mean values1981–2000 (20)MLM1k-means clustering, hierarchical clustering60
35[98]2021Entire territory of ChinaAT, RH, SR, W4National meteorological service National Meteorological Information CenterHourly values1961–2010 (50)BES1Transient system simulation
program software (TRNSYS) with 1 archetype (office)
36[44]2021Entire territory of ChinaTMY1SoftwareMedpha database of ChinaHourly values TMY BES, MLM2K-Means and agglomerative hierarchical clustering. DeST (designer’s simulation toolkits) with 1 archetype (20-story office)5
37[99]2018 EuropeAT,
RH, SR
3Web databaseEnergyPlus websiteHourly values TMY1982–1999 (18)KGM, MLM2k-means clustering, k-medoids clustering5
38[100] *2020 EuropeAT,
RH, SR
3Web databaseEnergyPlus websiteHourly values TMY1982–2000 (18)KGM, MLM2hierarchical clustering with Euclidean distances7
39[71]2020Entire territory of ChinaAT, RH, SR, AP4National meteorological service National Climate Center of China10 days mean values2004–2013 (10)MLM1K-nearest-neighbor and sparse subspace
representation.
5
40[77]2018 WorldAT, Pr2Climate modelWorldClim V1 and V2, and CHELSA V1.2, CHPclim V1; Table 1Monthly mean values1980–2016 (37)KGM1 30
41[69]2018Entire territory of TurkeyAT, Pr2National meteorological service Turkish
State Meteorological Service
1950–2010 (60)TCCM1 9
42[101]2016Part ofBrazil (State of Paraná)AT, rainfall, evapotranspiration3Climate modelEuropean Center for Medium-Range Weather Forecast (ECMWF) models Monthly mean values1989–2014 (25)KGM, TCCM, Camargo Climatic Classification3 3
43[102]2007 WorldAT and Pr2Web databaseGlobal Historical Climatology Network
(GHCN) version 2.0 dataset
Monthly mean values1909–1993 (70)KGM1 30
44[103]2019 WorldAT, Pr, solar irradiation3Web database“GPCCv2018” “CRU TS4.01”Monthly mean values1950–2016 (68)KGM1Köppen–Geiger-Photovoltaic (KGPV) 12
45[42] *2011 WorldAT, RH, TMY3SoftwareEcotect climate classification tool
(Autodesk Incorporated 2011)
TMY, monthly mean values BCM, BES2Standard psychometric charts with each location’s
actual temperature and RH, “SUNREL” software
(National Renewable Energy Laboratory 2010) with 3 archetypes
46[35]2020Entire territory of ChinaAT, DDs, Pr, SR, PW5National meteorological service National Climate Center (NCC)Daily mean value1997–2013 (17)DDM, MLM2Base temperatures: HDD 18 °C; CDD 10 °C, CD 26 °C; hierarchical clustering;17
47[104]2019Entire territory of ChinaAT, DDs2National meteorological service National Climate Center (NCC)Daily mean value1997–2013 (17)IJM, BES2Simulations with 1 archetype5
48[75]2016 WorldAT, Pr2Web databaseWorldClim global climate datasetMonthly mean values1950–2000 (50)MLM132 clustering methods, hierarchical clustering, partitioning around medoids5
49[105]2013 EuropeTMY1SoftwareMeteonormHourly values TMY BES1HAMBase and mathlab software with 1 archetype
50[106]2020Entire territory of AlgeriaTMY1Web databaseUnited States Department of
Energy
Hourly values TMY2004–2018 (15)BES1EnergyPlus simulations V8.9.0, energy demand and indoor-discomfort hours with typical multifamily social residential building
51[107] *2019Entire territory of BrazilAT, RH, SR, TMY4SoftwareEnergyPlus databaseHourly values TMY2005–2018 (13)BES, MLM2EnergyPlus simulations V8.9.0, annual building cooling thermal loads as indicators. 1 archetype. k-means clustering with the sum of squares (within SS) and Hubert index 5
52[108]2015Entire territory of ItalyDDs1National meteorological service Italian meteorological databaseMonthly mean values1978–2013 (35)DDM1Base temperatures: HDD 18 °C, HDD 20 °C, HDD 22 °C; CDD 22 °C, CD 24 °C, CDD 26 °C
53[109]2021Entire territory of SpainAT, DDs2National meteorological service State Meteorological
Agency (AEMET)
2015–2018 (4)CSIM, BES2HULC tool for simulation19
54[110]2015Entire territory of AlgeriaDDs1National meteorological service CNERIB, Réglementation thermique du bâtiment DDM1Base temperatures: HDD 18 °C; CDD 26 °C; territory is classified into climatic zones according to
the annual cost of energy consumption
7
55[111]2021Entire territory of BelarusAT, Pr, W3National meteorological service State Climate Cadastre of the Republic of Belarus (Belhy- dromet 2019)Daily values1971–2000 (30)BES1A historical simulation and an evaluation simulation
56[112]2013Entire territory of Czech Republic 14 1961–2000 (40)Quitt’s Climate Classification1 23
57[7]2017 Europe (Cyprus, France, Greece)
58[113]2017Part of Spain (Galicia)AT, RH2National meteorological service Monthly mean values(15)BCM2Givoni bioclimatic charts5
59[114]2021Entire territory of IrelandDDs1 Daily values2003–2017 (15)DDM1Base temperature: HDD 15, 5 °C
60[115]2015Entire territory of South KoreaDDs1National meteorological service Korea Meteorological AdministrationDaily values, 3 h values1981–2010 (30)DDM1 4
61[116] *2017Entire territory of PhilippinesPr1National meteorological service Philippine Atmospheric, Geophysical, and Astronomical Services Administration (PAGASA)Monthly mean values1961–2015 (55)MLM1K-means clustering, hierarchical clustering6
62 2002Entire territory of NigeriaAT, RH2 (20)MM1 9
63[117]2020Entire territory of NigeriaAT, RH2National meteorological service Meteorological center of NigeriaMonthly mean values(5)BCM1Olgyay charts5
64[118]2002Entire territory of VenezuelaAT, RH, Al3 IJM1Al correction5
65[119]1999Part of United States (Puerto Rico)AT, Pr2 Seasonal mean values1960–1990 (31)MLM1Principal component analysis, artificial neural networks (ANN)4
66[120]2010Entire territory of Dominican RepublicAT, Pr2National meteorological service ONAMET network, National Institute for Hydrologic Resources (Instituto Nacio- nal de Recursos Hidráulicos, or INDRHI)Monthly mean values1971–2000 (30)TCCM1 9
67[121]2018Entire territory of Dominican RepublicAT, RH2National meteorological service ONAMET network, National Institute for Hydrologic Resources (Instituto Nacio- nal de Recursos Hidráulicos, or INDRHI)30 min values1998–2016 (18)FDV1Frequency distribution of maximum and minimum values of AT and RH8
68[34]2021Part ofChina (cold climate zone)TMY1 Hourly values TMY BES, MLM2EnergyPlus simulation with 1 archetype, k-means clustering4
69[53]2022Entire territory of EthiopiaAT, RH, SR, TMY4Web database, climate model, softwareWorldClim repository, CRU CL v. 2.0: (A high-resolution data set of surface climate over global land areas), Meteonorm softwareMonthly mean values BES, MLM2K-means clustering, principal component analysis, Mahoney method, EnergyPlus simulation with 2 archetypes10
70[51]2020Part ofChileTMY1Climate modelthe Mesoscale Meteorological Model ver.5 (MM5)Hourly values TMY BES1Simulation with 1 archetype
71[52]2020Entire territory of ChinaAT, RH2National meteorological service National Meteorological Information Center 1984–2013 (30) MLM1Mahalanobis distance as an indicator for evaluating the distances between samples7
72[39]2022Part ofBrazil (semiarid region)AT, Pr, SR, W, PW5Web databaseWorld-Clim 2 Data PortalMonthly mean values1970–2000 (30)MLM1Principal component analysis, hierarchical clustering 3
73[122]2018Part ofChile (south part (La Araucanía, Los Ríos, and Los Lagos))DDs, SR2National meteorological service Ministry of Agriculture-National Agroclimatic NetworkHourly values2011–2015 (4)CSIM1Base temperatures: HDD 20 °C; CDD 20 °C3
74[123]2017Entire territory of SwedenPrimary energy consumption1 EBSM1Primary energy consumption (measured in kWhp/m2),3
75[22]2021Entire territory of SpainDDs1National meteorological service Spanish State Meteorological Agency (AEMET) (State Meteorological Agency-AEMET-Spanish Government, 2020)Hourly values2015–2018 (4)CSIM1Base temperatures: HDD 20 °C; CDD 20 °C12
76[124]2009Entire territory of ThailandAT1National meteorological service Department of MeteorologicalHourly values1981–1999 (18) 3
77[6]2012Entire territory of GreeceAT, SR2 Hourly values1961–1990 (30)BES1TRNSYS software simulations with 3 archetypes13
78[40]2021Part of Spain (Andalusia)TMY (EPW)1SoftwareMETEONORMEPW BES, MLM2Simulations with 8 archetypes, k-means clustering12
79[125]2016Part of (Catalonia)SpainPrimary energy consumption1 Catalan Institute of EnergyPrimary energy consumption1980–2008 (30)EBSM1Primary energy consumption (measured in kWhp/m2),3
80[126] *2021Entire territory of MexicoTMY (EPW)1SoftwareEnergyPlus EPW BES1Open Studio with 3 archetypes10
81[127]2021Entire territory of LibyaDDs1 Daily mean values DDM1Base temperatures: HDD 24 °C; CDD 18 °Ccontinuous
82[128]2014Entire territory of TurkeyAT1National meteorological service State Meteorology General Directorate (42)FDV1The outdoor temperature distributions 8
83[50]2021Entire territory of TurkeyWall insulation, fuel types, DDs3 MLM1Fuzzy c-mean clustering5
84[129] *2014Entire territory of NepalAT, RH, W3National meteorological service Department of Hydrology and MeteorologyTMY BCM1Givoni charts4
85[130]2017Entire territory of South KoreaAT1National meteorological service Korea Meteorological Administration (KMA) 2001–2010 (10)FDV1Graph pattern of the cumulative temperature density4
86[131]2011Entire territory of IranAT, RH, AP3 BCM1 4
87[132]2017Part of (Pampas)ArgentinaAT, RH, W, Pr, Al5National meteorological service National Meteorological Service (SMN, Argentina)Monthly mean values1960–2010 (50)MLM1Ward agglomerative hierarchical clustering method8
88[49]2021Entire territory of IranAT, RH2 1995–2014 (20)MLM, BCM2Givoni’s bioclimatic chart modified by Brown and Dekay19
89[133]2007Part of (San Luis Potosí, central–northeastern region of México)MexicoAT, Pr2National meteorological service México’s Comisión Nacional del Agua (CNA)Monthly mean values1940–1997 (28)KGM, MLM2Principal component analysis6
90[134]2019Entire territory of IndiaAT, RH, DDs3National meteorological service Indian Society of Heating Refrigerating and Air-conditioning Engineers (ISHRAE)Hourly weather data MLM1Hierarchical clustering8
91[135]2015Entire territory of IndiaAT, RH, Pr3Web databaseSEWRA and UNEP NASA’s Surface meteorologyRaster and shape file datasets1983–2005 (25)MM1 62
92[136]2019Part of (Kerala)IndiaAT, DHs, Al3SoftwareMeteonormTMY DDM, BES2Al correction3
93[137]2004Entire territory of ThailandAT, RH, Pr, SR, Al5National meteorological service Thai meteorological service 1990–2000 (10) Al correction
94[138]2021Entire territory of MoroccoAT, RH, Pr, SR4Web databaseThe Prediction of Worldwide Energy Resource (POWER) 1984–2017 (32)MLM1Hierarchical clustering, k-means clustering, support vector machine classifier (SVM-C)8
95[45]2022Entire territory of India
96[139] *2003
97[140] *2003Entire territory of United StatesAT, RH, DDs3 IJM, DDM2 17
98[141]2022Entire territory of EthiopiaAT, DDs2National meteorological service National Center for Environmental Prediction (NCEP) 1979–2013 (34)DDM1Heating degree-days (HDD) and cooling degree-days (CDD) with base temperature of 18.3 °C5
99[142]2006Entire territory of ChinaAT, RH2National meteorological serviceNational Meteorological Centre of ChinaDaily values1971–2000 (30)BCM1 9
100[143] **2014Territory of Eastern Africa (Tanzania, Kenya, Uganda)AT, RH2 BCM, MM2Givoni charts6
101[144] **1991Entire territory of EthiopiaAT, Pr, Al3 Annual mean values IJM1Al correction6
102[145]2020
103[24] ***2017
104[146] ****2007Entire territory of BoliviaAT, RH2National meteorological service National meteorological service (SENAMHI) 1970–2004 (35)BCM1Givoni bioclimatic charts, ABC software8
105[147] ****2020Entire territory of EthiopiaAT, RH, DDs3National meteorological service National Center for Environmental Prediction NMAE, National Meteorological Agency of Ethiopia 1974–2013 (30)DDM1Heating DDs (base 18.3 °C)5
* Conference paper. ** Book. *** Review paper. **** Thesis.
Table 2. CZB variables definitions.
Table 2. CZB variables definitions.
#Variable Group NameAbbreviationsVariables Included
1ATATDry-bulb temperature
Wet-bulb temperature
Temperature ranges
Seasonal and extreme temperatures
2Relative humidityRHRelative humidity
Moisture content
3Degree-daysDDsDegree-days
Degree-hours
4Solar radiationSRDirect solar radiation
Diffuse solar radiation
Global horizontal irradiation (GHI)
Sunshine duration
Daily clearness index
5PrecipitationPrRainfall
Snowfall
6WindWWind speed
Wind frequency
Wind direction
7Typical meteorological yearTMYSet of meteorological data (TMY, EPW, RMY, etc.)
8AltitudeAlAltitude
9Atmospheric pressureAPAtmospheric pressure
10The pressure of water vaporPWThe pressure of water vapor
Table 3. CZ methods definitions.
Table 3. CZ methods definitions.
#Name of a MethodAbbreviationsCriteria
1Machine learning methodsMLMClassification is based on clustering techniques, neural networks, support vector machines, sensitivity analysis, or principal component analysis
2Degree-days/-hours methodsDDMClassification is based DDs values only. OR If several variables are used in the classification, then DDs should be the primary variable
3Building energy simulationBESClassification is based on BES results
4Bioclimatic charts methodBCMClassification is based on Givoni, Lamberts, Milne, and Olgay charts with the combination of temperature and humidity as the main variables
5Köppen–Geiger methodKGMClassification is followed by the Köppen–Geiger system and is based on seasonal precipitation and temperature pattern
6Climate severity index methodCSIMClassification is based on the climate severity index (a site-specific value that defines the severity index of a specific climate) according to Formulas 4 and 5
7Interval judgment method (the complex combination of climate variables based on the repeatability of their elements)IJMThe classification is based on a combination of different variables with established limits (threshold) of variables for each zone
8Frequency distribution
of climate variable
FDVClassification is based on the different types of probability distributions of variable(s)
9Mahoney methodMMClassification is based on Mahoney tables
10Thornthwaite climate classification methodTCCMClassification is based on Thornthwaite climate classification
11Existing building stock performance methodEBSMClassification is based on actual data of building stock performance
12Heating or cooling indexHCIClassification is based on heating and cooling indexes. This index is commonly used to determine how ambient temperature, relative humidity, and radiation affect human comfort
13Other Quitt’s climate classification
Roriz method
The World Health Organization (WHO) classification method
Administrative division
Approximation and interpolation method (AIM)
Camargo climatic classification
Table 4. Authors working with different CZB methods.
Table 4. Authors working with different CZB methods.
AbbreviationsCases%First AuthorsReferences
MLM3434.7%Aliaga, Alrashed, Anas, Bai, Benevides, Bhatnagar, Bienvenido-Huertas, Deng, Erell, Falquina, Fovell, Lau, Malmgren, Mazzaferro, Netzel, Pernigotto, Pineda-Martínez, Praene, Roshan, Shi, Tükel, Unal, Walsh, Wan, Wang, Xiong, Yang, Zeleke, Zscheischler[10,23,25,27,34,35,39,40,44,46,49,50,52,53,71,72,74,75,80,84,87,93,94,95,96,97,99,100,107,119,132,133,134,138]
DDM2525.5%Abebe, Asfaw, Bai, Bawaneh, Briggs, D’Amico, De Rosa, Elmzughi, Ghedamsi, Mazzaferro, Muddu, Nair, Noh, Pusat, Rakshit, Ramon, Sánchez de la Flor, Tsikaloudaki, Verichev, Walsh, Xiong[9,23,25,27,32,35,43,46,79,81,85,86,90,108,110,114,115,127,136,140,141,147]
BES2525.5%Asimakopoulos, Bai, Bienvenido-Huertas, Carpio, Cory, D’Amico, Danilovich, Deng, Díaz-López, Kishore, Mazzaferro, Meng, Nair, Semahi, Tsikaloudaki, van Schijndeln, Verichev, Walsh, Wang, Xiong, Zeleke[6,25,27,32,34,40,41,42,44,46,48,51,53,79,81,89,104,105,106,107,109,111,136,153]
BCM1616.3%Bodach, Cory, da Casa Martín, Kishore, Lam, Mahmoud, Mobolade, Moradchelleh, Navarro, Rakoto-Joseph, Roriz, Roshan, Singh[42,48,49,76,80,82,91,92,113,117,131,142,146,154]
KGM1111.2%Alrashed, Aparecido, Ascencio-Vásquez, Beck, Mazzaferro, Peel, Pernigotto, Pineda-Martínez, Sarricolea, Zscheischler[46,72,73,77,96,99,100,101,102,103,133]
CSIM66.1%Carpio, Diaz-Lopez, Moral, Verichev[22,41,47,90,109,122]
IJM44.0%Bai, Briggs, Ferstl, Hobaica[104,118,140,144]
FDV44.0%Coskun, Felix, Khedari, Kim[88,121,128,130]
MM33.0%Ogunsote, Pawar, Zeleke[53,116,135]
TCCM22.0%Aparecido[101]
EBSM22.0%Gangolells, Hjortling[123,125]
HCI11.0%Wan[84]
Table 5. The most-cited publications in the review.
Table 5. The most-cited publications in the review.
#AuthorsTitleYearJournalCited byDocument TypeReference
1Peel M.C.Updated world map of the Köppen–Geiger climate classification2007Hydrology and Earth System Sciences5580Article[102]
2Beck H.E.Present and future Köppen–Geiger climate classification maps at 1 km resolution2018Scientific Data1091Article[77]
3Fovell R.G.Climate zones of the conterminous United States defined using cluster analysis1993Journal of Climate286Article[95]
4Unal Y.Redefining the climate zones of Turkey using cluster analysis2003International Journal of Climatology235Article[94]
5Wang H.Impact of climate change heating and cooling energy use in buildings in the United States2014Energy and Buildings193Article[89]
6Attia S.Overview and future challenges of nearly zero energy buildings (nZEB) design in Southern Europe2017Energy and Buildings156Article[7]
7Sarricolea P.Climatic regionalisation of continental Chile2017Journal of Maps121Article[73]
8Asimakopoulos D.A.Modeling the energy demand projection of the building sector in Greece in the 21st century2012Energy and Buildings115Article[6]
9Nguyen A.T.An investigation on climate responsive design strategies of vernacular housing in Vietnam2011Building and Environment88Article[190]
10Gangolells M.Energy mapping of existing building stock in Spain2016Journal of Cleaner Production79Article[125]
Table 6. Summary of papers for future climate scenarios.
Table 6. Summary of papers for future climate scenarios.
ReferenceCountry/RegionScenarioPredicted PeriodClimate Model NameScenario Type
[9]Entire territory ofBelgiumCurrent/Future2070–2098EC-Earth driven CPM for the Belgian domain
extended with land-surface scheme TERRA_URB
RCP 8.5
[10]Entire territory ofIranCurrent/Future2025, 2050, and 2075MAGICC and SCENGEN
[97] WorldCurrent/Future2081–2100CCSM
CSIRO-Mk3.6.0
MPI-ESM-MR
GFDL-CM3
GISS-E2-R
IPSL-CM5A-LR
MRI-CGCM3
HadGEM2-ES
RCP8.5
[77] WorldCurrent/Future2071–2100CMIP5 32 climate model projectionsRCP8.5
[103] WorldCurrent/Future2015-2100“SSP5-8.5” climate change scenario, created by the Institute
Pierre Simon Laplace (IPSL)
SSP5-8.5
[109]Entire territory ofSpainCurrent/Future2055
and 2085
RCP 4.5 and RCP
8.5
[110]Entire territory ofAlgeriaCurrent/Future2040
[111]Entire territory ofBelarusCurrent/Future2021–2040, 2041–2060, 2061–2080, and 2081–209992 regional circulation model (RCM) from EURO-CORDEX RCM ensembleRCP2.6, RCP4.5, and RCP8.5
[22]Entire territory ofSpainCurrent/Future2055 and 2085IPCC AR5RCP2.6 and RCP8.5
[6]Entire territory ofGreeceCurrent/Future2041–2050 and 2091–2100IPCC AR5 12 different regional climate models of the European ENSEMBLES projectRCP2.6, RCP4.5, and RCP8.5
[40]Part ofSpain (Andalusia)Current/Future2050 and 201018 climate models included in the 2007 IPCC reportA2 scenario of the Special Report on Emissions Scenarios (SRES)
[89]Entire territory ofUnited StatesFuture2020,
2050, and 2080
HadCM3RCP2.6, RCP4.5, and RCP8.5
[51]Part ofChileFuture2050–2065IPCC AR5RCP2.6 and RCP8.5
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Remizov, A.; Memon, S.A.; Kim, J.R. Climate Zoning for Buildings: From Basic to Advanced Methods—A Review of the Scientific Literature. Buildings 2023, 13, 694. https://doi.org/10.3390/buildings13030694

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Remizov A, Memon SA, Kim JR. Climate Zoning for Buildings: From Basic to Advanced Methods—A Review of the Scientific Literature. Buildings. 2023; 13(3):694. https://doi.org/10.3390/buildings13030694

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Remizov, Alexey, Shazim Ali Memon, and Jong R. Kim. 2023. "Climate Zoning for Buildings: From Basic to Advanced Methods—A Review of the Scientific Literature" Buildings 13, no. 3: 694. https://doi.org/10.3390/buildings13030694

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