Solar Radiation and Climate Change: Direct and Indirect Interconnections

A special issue of Applied Sciences (ISSN 2076-3417). This special issue belongs to the section "Earth Sciences".

Deadline for manuscript submissions: closed (31 March 2024) | Viewed by 843

Special Issue Editor


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Guest Editor
1. Atmospheric Research Team, Institute of Environmental Research and Sustainable Development, National Observatory of Athens, Lofos Nymphon, GR-11810 Athens, Greece
2. Soft Energy Systems and Environmental Protection Laboratory, Department of Mechanical Engineering, University of West Attica, P. Ralli & Thivon 250, GR-12244 Egaleo, Greece
Interests: solar radiation; atmospheric aerosols; atmospheric turbidity; daylighting; climatology; meteorology; climate change
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Special Issue Information

Dear Colleagues,

Solar radiation plays a crucial role in driving the Earth’s climate system and is closely linked to climate change. The inter-relationship between solar radiation and the climate system is rather complex because the former directly and indirectly influences our climate. The energy from the Sun (in the UV, VIS, and IR bands) passes through the Earth’s atmosphere and reaches its surface, thus influencing various climatic processes.

This Special Issue aims to collect new research and findings regarding solar radiation and climate interconnections.

Therefore, the scope of this Special Issue includes measurements, methods, and techniques that can provide advanced knowledge on how solar radiation (or solar energy) affects our climate (and consequently contributes to climate change) in both a negative and positive manner.

Dr. Harry D. Kambezidis
Guest Editor

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Keywords

  • solar radiation
  • solar energy
  • solar radiation and energy balance
  • Earth’s climate system
  • climate change
  • solar variability
  • greenhouse effect
  • atmospheric aerosols
  • global warming
  • climate models
  • solar energy and weather modification

Published Papers (1 paper)

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Research

13 pages, 550 KiB  
Article
Trends from 30-Year Observations of Downward Solar Irradiance in Thessaloniki, Greece
by Athanasios Natsis, Alkiviadis Bais and Charikleia Meleti
Appl. Sci. 2024, 14(1), 252; https://doi.org/10.3390/app14010252 - 27 Dec 2023
Viewed by 527
Abstract
The shortwave downward solar irradiance (SDR) is an important factor that drives climate processes and energy production and can affect all living organisms. Observations of SDR at different locations around the world with different environmental characteristics have been used to investigate its long-term [...] Read more.
The shortwave downward solar irradiance (SDR) is an important factor that drives climate processes and energy production and can affect all living organisms. Observations of SDR at different locations around the world with different environmental characteristics have been used to investigate its long-term variability and trends at different time scales. Periods of positive trends are referred to as brightening periods and of negative trends as dimming periods. In this study we have used 30 years of pyranometer data in Thessaloniki, Greece, to investigate the variability of SDR under three types of sky conditions (clear-, cloudy- and all-sky). The clear-sky data were identified by applying a cloud screening algorithm. We have found a positive trend of 0.38%/year for all-sky, ∼0.1%/year for clear-sky, and 0.41%/year for cloudy conditions. The consistency of these trends, their seasonal variability, and the effect of the solar zenith angle have also been investigated. Under all three sky categories, the SDR trend is stronger in winter, with 0.7, 0.4, and 0.76%/year, respectively, for all-, clear-, and cloudy-sky conditions. The next larger seasonal trends are in autumn—0.42 and 0.19%/year, for all and cloudy skies, respectively. The rest of the seasonal trends are significant smaller, close to zero, with a negative values in summer, for clear and cloudy skies. The SDR trend is increasing with increasing solar zenith angle, except under cloudy skies, where the trend is highly variable and close to zero. Finally, we discuss shorter-term variations in SDR anomalies by examining the patterns of the cumulative sums of monthly anomalies from the climatological mean, both before and after removing the long-term trend. Full article
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