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Article

Bayesian Optimization and Hierarchical Forecasting of Non-Weather-Related Electric Power Outages

by
Olukunle O. Owolabi
1,* and
Deborah A. Sunter
1,2,3,4,5,*
1
Department of Mechanical Engineering, Tufts University, Medford, MA 02155, USA
2
Department of Civil and Environmental Engineering, Tufts University, Medford, MA 02155, USA
3
Department of Computer Science, Tufts University, Medford, MA 02155, USA
4
Center for International Environment and Resource Policy, Tufts University, Medford, MA 02155, USA
5
Tufts Institute of the Environment, Tufts University, Medford, MA 02155, USA
*
Authors to whom correspondence should be addressed.
Energies 2022, 15(6), 1958; https://doi.org/10.3390/en15061958
Submission received: 20 January 2022 / Revised: 1 March 2022 / Accepted: 2 March 2022 / Published: 8 March 2022
(This article belongs to the Section F1: Electrical Power System)

Abstract

:
Power outage prediction is important for planning electric power system response, restoration, and maintenance efforts. It is important for utility managers to understand the impact of outages on the local distribution infrastructure in order to develop appropriate maintenance and resilience measures. Power outage prediction models in literature are often limited in scope, typically tailored to model extreme weather related outage events. While these models are sufficient in predicting widespread outages from adverse weather events, they may fail to capture more frequent, non-weather related outages (NWO). In this study, we explore time series models of NWO by incorporating state-of-the-art techniques that leverage the Prophet model in Bayesian optimization and hierarchical forecasting. After defining a robust metric for NWO (non-weather outage count index, NWOCI), time series forecasting models that leverage advanced preprocessing and forecasting techniques in Kats and Prophet, respectively, were built and tested using six years of daily state- and county-level outage data in Massachusetts (MA). We develop a Prophet model with Bayesian True Parzen Estimator optimization (Prophet-TPE) using state-level outage data and a hierarchical Prophet-Bottom-Up model using county-level data. We find that these forecasting models outperform other Bayesian and hierarchical model combinations of Prophet and Seasonal Autoregressive Integrated Moving Average (SARIMA) models in predicting NWOCI at both county and state levels. Our time series trend decomposition reveals a concerning trend in the growth of NWO in MA. We conclude with a discussion of these observations and possible recommendations for mitigating NWO.

1. Introduction

Power outages demonstrate a failure in the proper functioning of an electrical distribution system [1,2,3,4]. These outage events can result in substantial financial losses [5,6,7], such as food spoilage [8,9] or a serious health emergency in a health facility [10], especially when back-up sources of generation fail [11]. Developing a robust outage risk mitigation strategy [12,13] is important for utility managers to formulate protective and preventive measures that reduce the occurrence of electric outages. Outage forecasting models are a useful tool for uncovering historical and future trends of outage events and can, therefore, guide outage preventive and mitigation strategies [14].
The cause of an outage influences its magnitude or severity. Outages as a result of extreme weather events (Extreme Weather Outages, EWO), such as a storm or high winds, may result in a loss of power for numerous customers at a time [15,16,17]. Outages unassociated with adverse weather events (Non-extreme weather outages or non-weather related outages, NWO) often affect a smaller proportion of electricity customers at a time, such as those emanating from the ecology domain as a result of an animal disturbance [18,19,20]. While in most cases (and as shown in Table 1), the average and median values of the number of customers affected and the duration of outages from EWO often exceed those of NWO, these NWOs have a significant cumulative effect on the electrical distribution grid. As can be seen in the summary statistics in Table 1, the total number of outages and total number of customers affected as a result of NWO in MA exceed those of EWO within the studied 6-year period from 2013–2018. However, it is important to note that the statistics presented in Table 1 are only valid for the study location and period. Large EWO are less frequent and therefore short—term comparison (as in Table 1) gives only partial information about the long term effect of EWO relative to NWO.
The majority of outage forecasting models in literature have focused on EWO [14,16,22,23,24,25,26,27,28,29,30,31,32,33,34,35,36,37] while neglecting the impact of NWO whose long-term cumulative effects are substantial. There have been a few NWO studies that have focused on subsets of these outages, such as animal and vegetation related outages. For example, the prediction and analysis of animal related outages have been explored using a combination of statistical and advance machine learning techniques [18,20,38]. Also, similar predictive techniques for vegetation related outages (as a result of tree growth) have been explored [39].
This study explores NWO and aims to understand trends in these outages that may be useful in improving electrical distribution grid reliability. The specific contribution of this study include: (1) development of a quantitative metric for NWO that can aid the understanding and quantification of these outages, (2) development of a time series forecasting framework that exposes critical trends and seasonal patterns in NWO, and (3) improvement of the state-of-the-art prediction performance using proposed Bayesian and hierarchical methods. Based on the study methodology (Figure 1), we develop a robust time series forecasting framework for NWO at the state and county level. Our case study is based on the state of Massachusetts (MA) with outage data from 2013–2018 [21]. After deriving a quantitative count-based metric (Non-weather Outage Count Index, NWOCI) for NWO and leveraging advanced data preprocessing tools in Kats [40], a Bayesian optimization method with a Prophet model [41] is used for the state level forecast and a hierarchical Prophet bottom-up approach is used to produce the county level forecasts. Bayesian optimization helps to improve model performance and reduce computation time [42], while hierarchical models are the optimal choice for multi—time series forecasting, especially for grouped or subdivided data [43] (in this case, county level forecasting for multiple counties in the study region—MA). A comparative analysis evaluates the performance of the proposed models relative to other SARIMA and Prophet Bayesian and hierarchical models. The forecast trend and seasonality are also analysed to better understand observed historical and future NWO trends. The complete end-to-end methodology used in this study is describe in Figure 1.

2. Methods

2.1. Data Collection

2.1.1. Outage Data

The state of MA was selected for this study based on the availability of outage reports across the state between 2013–2018. These reports are a component of the Emergency Response plan filed by each of the three major utilities in MA—National Grid, Eversource Energy, and UNITIL corporation—and contain information on the date, time, location, and cause of the outage [21].
Data preprocessing was done to ensure data integrity and develop consistent daily time series. First, data verification procedures were used to address problems such as typographical errors or mismatch in the location reported for the outage. Details of these procedures can be found in the Appendix A.1. Next, steps were taken to obtain a consistent, ready-to-use, daily time series. First, days with no outages in the aggregated time series are replaced with zeros. Then outlier values were treated using the outlier detector algorithm in the Kats toolkit [40] using the standard 1.5 × (IQR) outlier designation and replaced with the interpolated value.

2.1.2. Weather Data

Wind speed data (including gust speed) between 2013–2018 (corresponding to the range of the outage data), was collected from all 23 operating weather stations in MA (Figure 2) at hourly level from the National Oceanic and Atmospheric Administration (NOAA) database via the climate data online local climatological data repository [44]. The wind gusts data are only reported when there is a short-term wind speed (typically 20 s or less) that both exceeds 16 knots (about 18 mph) and exceeds the average wind speed by at least 9–10 knots (10–11 mph) [45]. Whenever there is a gust speed, we replace the average wind speed value at that hour with the gust speed to account for the influence of these short term extreme winds. The hourly wind speed were matched with the raw outage data corresponding to the starting time (hour) and location (shortest euclidean distance) of the outage event and then used to delineate extreme weather outage instances.

2.2. Non-Weather Outage Count Index (NWOCI)

We classify an outage as an NWO if the outage did not occur during instances of high wind threat and other adverse weather conditions including precipitation, lightning, thunderstorm, and snow. First, we begin with classifying Extreme Weather Outages (EWO) based on two indicators:
(1)
Categorical classification of the outage event—adverse weather conditions (which captures all other extreme weather events including Wind, Precipitation, Snow, Lightning, and Thunderstorm)
(2)
Wind threat threshold: If the wind speed exceeds 40 mph—a threshold above which it poses a high or extreme threat, according the National Oceanic and Atmospheric Administration (NOAA) as seen in Table 2 [46], the outage is categorized as an EWO. We use this wind threat to further validate our classification of EWO while capturing potential mis-classified outages.
We then define the daily Non-extreme Weather Outage Count Index (NWOCI) as the total number of NWOs each day in the state and each county, respectively. This is calculated by subtracting the number of outages classified as EWO from the total number of reported outages. It is important to note that each NWO is counted equally, regardless of outage duration and the number of customers affected. As seen in Table 1, the duration and number of affected customers is typically modest for NWO relative to EWO. The focus of this study is on the frequency of NWO and not the magnitude of these events.

2.3. Prophet Model

Prophet [41], an open-source software released by Facebook’s Core Data Science team, was used for time series forecasting. Prophet uses a decomposable model architecture including the following model elements: trend g, seasonality s, and holidays h.
y ( t ) = g ( t ) + s ( t ) + h ( t ) + ε t
In this study, we use the linear trend model specification in Prophet given as:
g ( t ) = k t + m
where k is the growth rate and m is the offset parameter; details on the Prophet model can be found in [47].

2.4. Bayesian Optimization Using True Parzen Estimator (TPE)

In this study, we incorporated Bayesian optimization into the Prophet time series model, using the True Parzen Estimator (TPE) [48]. TPE is a type of Sequential Model Based Optimization (SMBO) [49] technique that uses the Bayesian approach in an effort to reduce computational time. The implementation of TPE Bayesian optimization in this study was carried out using the hyperopt software package [48] in the Python programming language. We call this integrated model, that uses the Prophet-based objective function with TPE, Prophet-TPE. The steps in developing Prophet-TPE (as illustrated in Figure 3) include:
  • Search domain: First, the domain over which the hyperparameter search will be conducted is defined. For the first iteration, a random combination of hyperparameters within the ranges set forth in Table A1, is used. In each subsequent iteration, the combination of hyperparameters is adjusted using the probability distribution based on the performance of other combinations used in previous iterations.
  • Objective function: The objective function takes in a combination of hyperparameters and output the 5-fold expanding window cross-validated root mean squared error (RMSE) to be minimized over the Prophet model one-year ahead forecast. Unlike a rolling window that moves the upper and lower bound with each time step, the expanding window fixes the lower bound; thus, the amount of data considered incrementally increases (expands) with each time step. The cross validation was performed using the built-in cross validation diagnostic in Prophet [41]. A model is then built to evaluate the objective function. This model is called the surrogate model.
  • History: In Prophet-TPE each iteration forms the history. This set of historical information on the performance of a set of hyperparameters on the actual objective (minimizing the Prophet model’s error) is used to construct the probability distributions.
  • Probability distribution: This is a mapping of the probability of error, y, for a combination of hyperparameters, x.
  • Evaluation criteria: This is the method for obtaining the next best set of hyperparameters. The evaluation criteria is called the Expected Improvement (EI) which is given as [48]:
    E I y * ( x ) = y ( y * y ) P ( y | x ) d y
    P ( y | x ) = P ( x | y ) P ( y ) P ( x )
    P ( x | y ) = l ( x ) , i f y < y * g ( x ) , i f y y *
    where g ( x ) and l ( x ) are probability distributions and y* is the current best set of model hyperparameters in the history (lowest RMSE). The aim is to choose the next hyperparameter combinations that maximizes EI.
  • Update history: The set of distributions developed from historical information forms the basis of a series of iterative improvement for the surrogate model until the maximum number of iterations ( n = 10 ) is reached.

2.5. Hierarchical Forecasting Model with Bottom-Up Approach

Hierarchical forecasting is a way to obtain disaggregated, multi-time series forecast at finer scales that must add up to the whole [50]. This approach may improve forecast performance while reducing dis-aggregation error. In the bottom up approach, forecasts are obtained for lower levels in the hierarchy with upward aggregation to reconcile the forecast with the upper levels of the hierarchy. We represent the outage data as a hierarchical tree, with a focus on the county-level forecasts and reconciliation at the state level, as seen in Figure 4. We then propose a Prophet model with bottom up approach (Prophet-BU) for forecasting county-level NWOCI. The Prophet-BU forecasting approach was implemented in this study using the scikit-hts software package [51] in the Python programming language.

2.6. Performance Evaluation

The performance of the proposed models is evaluated using the RMSE to assess the difference between the daily forecasted prediction of NWOCI and the actual NWOCI at the state level for Prophet-TPE and the county level for Prophet-BU. Since we have time series data, the data are divided sequentially into train and test with 2013–2017 NWOCI used for training and 2018 data used for testing for both the Prophet-TPE (state level forecast) and the Prophet-BU (county level forecast). The default interval width of 0.8, representing the 80% confidence interval, was used to understand the forecast uncertainty of the proposed models.
The performance of the proposed models, Prophet-TPE and Prophet-BU, is compared with other Bayesian and hierarchical model combinations. For the state-level forecast, the proposed Prophet-TPE method is compared with other Seasonal Autoregressive Integrated Moving Average (SARIMA) and Prophet Bayesian models. These include: SARIMA-TPE, SARIMA-Anneal (SARIMA model with simulated annealing), and Prophet-Anneal (Prophet with simulated annealing). For the county-level forecast, the proposed Prophet-BU model is compared with other Prophet and SARIMA heirachical forecasting models. These include the Prophet and SARIMA model in combination with each of the following: AHP (Average Historical Proportion—top down), OLS (Ordinary Least Square revision), WLSS (Structurally Weighted Least Squares revision), FP (Forecasted Proportions—top down), and PHA (Proportion of Historical Averages—top down). A complete list of the models used in the performance evaluation is shown in Figure 5.

3. Results and Finding

The result for the state level forecast (Table 3) shows the performance of the Prophet-TPE in comparison with other models. The optimal hyperparameter values found for the Prophet-TPE and other models are given in Table A2. We observed that the proposed Prophet-TPE gives the best prediction for NWOCI at the state level. The Prophet-TPE forecast results can be seen in Figure 6. A decomposition of the forecast Prophet-TPE trend (Figure 7) reveals a positive linear growth trend in average NWOCI representing a 100% increase from 2013–2019 (from 17 in 2013 to 34 in 2019). The seasonal decomposition plot of the Prophet-TPE model forecast shows the temporal patterns of NWOCI with a peak in the summer months (July peak).
For the county level Prophet-BU model, we observed an improved performance in the proposed model relative to other hierarchical and Prophet forecasting models (Table 4), indicating that the proposed Prophet-BU model better captures the temporal patterns of NWOCI at the county level. As an example, the forecast result for Middlesex county using Prophet-BU model is shown in Figure 8. In the trend decomposition plot for Prophet-BU’s Middlesex county forecast, we also observe a linear growth in NWOCI in the county in 2013–2018 (Figure 9). The seasonal decomposition plot also shows a summer peak in NWO in Middlesex county. The forecast and trend for all remaining 13 counties is shown in Figure A1, Figure A2, Figure A3, Figure A4, Figure A5, Figure A6, Figure A7, Figure A8, Figure A9, Figure A10, Figure A11, Figure A12 and Figure A13. Note that the performance of the Prophet-BU model (like any other time series model) varies depending on the amount of data available. Some counties as shown in Figure A1, Figure A2, Figure A3, Figure A4, Figure A5, Figure A6, Figure A7, Figure A8, Figure A9, Figure A10, Figure A11, Figure A12 and Figure A13 have very sparse data while some have more data points (e.g., Middlesex county) and, therefore, give more robust forecasts. A table of the performance of the Prophet-BU model (RMSE) across counties is given in Table A3.

4. Discussion

As shown in Figure 10, the three main causes of NWO are: (1) failed equipment, (2) tree contact (in normal weather condition), and (3) animals.
Failed equipment accounts for 33% of all NWOs in MA (Figure 10). This is similar to national estimates. According to a US Department of Energy study, 30% of all non-weather related outages in the United States are a result of failed equipment [52]. Equipment failure is a common problem in electrical distribution systems and can emanate from several electrical components e.g., conductor lines, load breakers, transformers, etc. Much of these outages equipment failure can be attributed to the aging electric infrastructure [53]. The summer peak observed in the NWOCI seasonal decomposition plot (Figure 7) may be attributed to high demand for air conditioning in the summer. The increased electrical load and stress on the grid may ultimately lead to more electrical equipment failures.
Tree contact as a result of vegetation growth is also a major problem in the electrical distribution grid. While tree contact is most prevalent in adverse weather outage events [54,55], there are tree contacts that occur even in normal weather conditions [56]. During the study period, 28% of NWOs in MA were a result of tree contact (Figure 10).
Animal-caused outages represent about 17% of NWO in MA (Figure 10). Squirrels and other animals chew electrical conductors and can cause a short-circuit leading to electric power outages [18,57,58]. Birds are a leading cause of overhead distribution outages in the United States as a result of their roosting, nesting, and breeding activities [59,60]. Animal interference may attribute to the observed summer peak in NWOCI (Figure 7) since there is an increased presence of migratory animals and the summer weather is more conducive for increased animal activity.

5. Conclusions

Unlike previous studies that focus on extreme weather outage (EWO) prediction, we highlighted the importance of capturing non-extreme weather outages (NWO), which occur more frequently and thus have substantial cumulative effect on the electrical distribution grid. We introduced a metric to quantify NWO (Non-extreme Weather Outage Count Index, NWOCI) and then proposed forecasting models to predict NWOCI at both state and county levels. We show that our proposed models outperform other Bayesian and hierarchical forecasting models in predicting NWOCI. Our proposed state-level model (Prophet-TPE) and county-level model (Prophet-BU) outperformed other models by a reduction in RMSE between 2–22% and 6–59%, respectively.
The time series trend decomposition for both proposed models shows an upward trend in NWOCI indicating an increasing frequency of NWOs in MA. This reinforces the importance of developing preventive measures by stakeholders and utility managers that capture not just the EWO but also those occurring from non-extreme weather events, such as those caused by failed equipment, tree contact in normal weather conditions, and animals. These measures could include:
  • Efforts to curb equipment failure (the leading cause of non-weather outage) by identifying weaknesses in the distribution grid and high-risk targets for predictive maintenance [52].
  • Prediction models that can forecast trends in vegetation growth and thus enable strategic tree trimming measures to be put in place.
  • Exploring the feasibility of underground power line solutions. Undergrounding electrical wires could be a solution especially for NWO which originate from animal interference. However, more research is needed on the cost-benefit tradeoff of this strategy.
  • Monitoring systems (which may be put in place by utilities) to track the rate of growth of NWOs. Such systems may reveal underlying causes of the problem and aid the development of manageable short and long term mitigation plans.

Author Contributions

Conceptualization: O.O.O.; Methodology: O.O.O.; Investigation: O.O.O.; Visualization: O.O.O.; Data Curation: O.O.O.; Formal Analysis: O.O.O.; Funding acquisition: D.A.S.; Project administration: O.O.O. and D.A.S.; Supervision: D.A.S.; Writing—original draft: O.O.O.; Writing—review & editing: O.O.O. and D.A.S. All authors have read and agreed to the published version of the manuscript.

Funding

NSF Harnessing the Data Revolution (HDR) program, “Collaborative Research: Predictive Risk Investigation SysteM (PRISM) for Multi-layer Dynamic Interconnection Analysis” (#1940176).

Data Availability Statement

Raw data can be found here: https://github.com/Qunlexie/bayesian-and-hierachical-forecasting-for-power-outages (accessed on 19 December 2021).

Conflicts of Interest

The authors declare no conflict of interest.

Appendix A

Appendix A.1. Outage Data Prepossessing

The initial data preprocessing involves data integrity and data verification procedures to address problems such as typographical errors or mismatch in the location reported for the outage. The data issues that were addressed during preprocessing include:
  • Missing Data: Missing data in the city or towns feature were filled by locating the street information (where available) on Google Maps [61]. Out of 138,153 observations, three had city/towns found in another state and two had no recorded data for city, town, or street. These observations were removed.
  • Zero values: Data points with zero customers affected or duration of outages were removed from our analysis. For example, utilities may report on failed equipment even if that failure didn’t result in customers losing power (e.g., power flickers). Since there is no realized outage for these observations, they are removed from the analysis.
  • Typographical errors, extra spaces, and inconsistent names: A thorough feature inspection was carried out to ensure that the feature elements were consistent throughout. For example, typographical errors in street names and cities or towns were addressed using Google Maps [61].

Appendix A.2. Computational Details

Appendix A.2.1. Software

The complete list of software used for the study includes:
  • Kats: Kats v 0.1.0 [40] was used for the time series preprocessing to ensure a consistent time series data before developing the Bayesian and hierarchical forecasting models.
  • Prophet: Prophet v 1.0.1 [41] was used to implement the overarching Prophet forecasting model which served as a backbone for all the proposed Bayesian and hierarchical time series in this study.
  • Scikit hts: Scikit hts v 0.3.0 [51] was used to implement the hierarchical forecasting models.
  • Hyperopt: Hyperopt v 0.2.7 [62] was used to implement the Bayesian optimization models.

Appendix A.2.2. Computational Time and Efficiency

In this study we have applied Bayesian and hierarchical models to the NWO prediction problem. While the comparison of the time complexity of these Bayesian models with other search models (random search or grid search) is beyond the scope of this article, this has been extensively studied to buttress the efficiency and computational efficiency of Bayesian models [48,62,63]. The Bayesian optimization methods explored in this study are known to be among the most efficient in terms of obtaining the optimal set of hyperparameters by intelligently using information on the performance of hyperparameters from the training process.

Appendix A.3. Tables

Table A1. Hyperparameter search domain for the Prophet and SARIMA models.
Table A1. Hyperparameter search domain for the Prophet and SARIMA models.
ModelSearch Domain
Prophet‘changepoint_prior_scale’: [0.0001, 0.0005, 0.001, 0.005],
‘changepoint_range’: [0.8, 0.85, 0.9, 0.95],
‘seasonality_mode’: [’additive’, ’multiplicative’],
‘seasonality_prior_scale’: [0.01, 0.1, 1.0, 10.0],
‘yearly_seasonality’: [True, False]
SARIMA‘d’: [1, 2], ‘p’: [1, 2, 3, 4, 5], ‘q’: [1, 2, 3, 4, 5],
‘seasonal_order’: [(1, 0, 1, 7), (1, 0, 2, 7), (2, 0, 1, 7), (2, 0, 2, 7), (1, 1, 1, 7), (0, 1, 1, 7)],
‘trend’: [“n”, “c”, “t”, “ct”]
Table A2. Hyperparameter results for state-level NWOCI forecast showing the optimal hyperparameter values for each of the four Bayesian Prophet and SARIMA models.
Table A2. Hyperparameter results for state-level NWOCI forecast showing the optimal hyperparameter values for each of the four Bayesian Prophet and SARIMA models.
ModelHyperparameters
Prophet-TPE‘changepoint_prior_scale’: 0.0001,
‘changepoint_range’: 0.9,
‘seasonality_mode’: ‘additive’,
‘seasonality_prior_scale’: 10.0,
‘yearly_seasonality’: True
Prophet-Anneal‘changepoint_prior_scale’: 0.005,
‘changepoint_range’: 0.85,
‘seasonality_mode’: ‘multiplicative’,
‘seasonality_prior_scale’: 0.1,
‘yearly_seasonality’: True
SARIMA-TPE‘d’: 1, ‘p’: 1, ‘q’: 3,
‘seasonal_order’: (2, 0, 2, 7), ‘trend’: ‘t’
SARIMA-Anneal‘d’: 1, ‘p’: 1, ‘q’: 5,
‘seasonal_order’: (1, 0, 1, 7), ‘trend’: ‘t’
Table A3. Performance of the Proposed Prophet BU model for each county in MA.
Table A3. Performance of the Proposed Prophet BU model for each county in MA.
RMSE
Barnstable3.63
Berkshire2.44
Bristol14.10
Dukes2.44
Berkshire0.41
Essex3.18
Franklin1.98
Hampden3.97
Hampshire1.57
Middlesex59.65
Nantucket0.22
Norfolk3.86
Plymouth4.04
Suffolk5.56
Worcester4.65

Appendix A.4. Figures

Figure A1. Left: One year forecast result (2018 test data) from Prophet-BU Model for Barnstable county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Barnstable county in MA.
Figure A1. Left: One year forecast result (2018 test data) from Prophet-BU Model for Barnstable county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Barnstable county in MA.
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Figure A2. Left: One year forecast (2018 test data) from Prophet-BU Model for Berkshire county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Berkshire county in MA.
Figure A2. Left: One year forecast (2018 test data) from Prophet-BU Model for Berkshire county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Berkshire county in MA.
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Figure A3. Left: One year forecast (2018 test data) from Prophet-BU Model for Bristol county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Bristol county in MA.
Figure A3. Left: One year forecast (2018 test data) from Prophet-BU Model for Bristol county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Bristol county in MA.
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Figure A4. Left: One year forecast (2018 test data) from Prophet-BU Model for Dukes county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Dukes county in MA.
Figure A4. Left: One year forecast (2018 test data) from Prophet-BU Model for Dukes county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Dukes county in MA.
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Figure A5. Left: One year forecast (2018 test data) from Prophet-BU Model for Essex county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Essex county in MA.
Figure A5. Left: One year forecast (2018 test data) from Prophet-BU Model for Essex county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Trend decomposition from Prophet-BU Model for Essex county in MA.
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Figure A6. Left: One year forecast (2018 test data) from Prophet-BU Model for Franklin county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
Figure A6. Left: One year forecast (2018 test data) from Prophet-BU Model for Franklin county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
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Figure A7. Left: One year forecast (2018 test data) from Prophet-BU Model for Hamphsire county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
Figure A7. Left: One year forecast (2018 test data) from Prophet-BU Model for Hamphsire county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
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Figure A8. Left: One year forecast (2018 test data) from Prophet-BU Model for Hampden county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
Figure A8. Left: One year forecast (2018 test data) from Prophet-BU Model for Hampden county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
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Figure A9. Left: One year forecast (2018 test data) from Prophet-BU Model for Nantucket county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
Figure A9. Left: One year forecast (2018 test data) from Prophet-BU Model for Nantucket county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
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Figure A10. Left: One year forecast (2018 test data) from Prophet-BU Model for Norfolk county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
Figure A10. Left: One year forecast (2018 test data) from Prophet-BU Model for Norfolk county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
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Figure A11. Left: One year forecast (2018 test data) from Prophet-BU Model for Franklin county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue represents region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
Figure A11. Left: One year forecast (2018 test data) from Prophet-BU Model for Franklin county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue represents region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
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Figure A12. Left: One year forecast (2018 test data) from Prophet-BU Model for Suffolk county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
Figure A12. Left: One year forecast (2018 test data) from Prophet-BU Model for Suffolk county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). Right: Corresponding trend decomposition from Prophet-BU Model.
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Figure A13. Left: One year forecast (2018 test data) from Prophet-BU Model for Worcester county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). The red dotted lines show the time series change point delineated by the prophet model. Right: Corresponding trend decomposition from Prophet-BU Model.
Figure A13. Left: One year forecast (2018 test data) from Prophet-BU Model for Worcester county in MA. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017). The red dotted lines show the time series change point delineated by the prophet model. Right: Corresponding trend decomposition from Prophet-BU Model.
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Figure 1. Flow chart of methodology used for this study.
Figure 1. Flow chart of methodology used for this study.
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Figure 2. Weather stations in MA where wind speed data was collected. Source: map was developed based on weather station data obtained from NOAA climate data repository [44].
Figure 2. Weather stations in MA where wind speed data was collected. Source: map was developed based on weather station data obtained from NOAA climate data repository [44].
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Figure 3. Optimization methodology of the Bayesian True Parzen Estimator with the Prophet-based objective function (Prophet-TPE).
Figure 3. Optimization methodology of the Bayesian True Parzen Estimator with the Prophet-based objective function (Prophet-TPE).
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Figure 4. Hierarchical representation of outages.
Figure 4. Hierarchical representation of outages.
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Figure 5. Performance Evaluation of the proposed Prophet-TPE and Prophet-BU models with model combinations of Prophet and SARIMA Bayesian and hierarchical forecasting models.
Figure 5. Performance Evaluation of the proposed Prophet-TPE and Prophet-BU models with model combinations of Prophet and SARIMA Bayesian and hierarchical forecasting models.
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Figure 6. One year forecast result (2018 test data) from Prophet-TPE Model. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values (daily state level NWOCI) in the training data (2013–2017).
Figure 6. One year forecast result (2018 test data) from Prophet-TPE Model. N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values (daily state level NWOCI) in the training data (2013–2017).
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Figure 7. Top: Forecast components (trend and seasonality) with the Prophet-TPE model for the state of MA. N.B: The top panel shows the forecast trend of NWOCI based on the Prophet-TPE state level forecast. The bottom panel shows the decomposed yearly seasonal pattern of NWOCI.
Figure 7. Top: Forecast components (trend and seasonality) with the Prophet-TPE model for the state of MA. N.B: The top panel shows the forecast trend of NWOCI based on the Prophet-TPE state level forecast. The bottom panel shows the decomposed yearly seasonal pattern of NWOCI.
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Figure 8. One year forecast result (2018 test data) from Prophet-BU Model for Middlesex county in MA (corresponding NWOCI RMSE value for Middlessex county is 59.6). N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017).
Figure 8. One year forecast result (2018 test data) from Prophet-BU Model for Middlesex county in MA (corresponding NWOCI RMSE value for Middlessex county is 59.6). N.B: The solid blue line shows the average forecast while the solid red line shows the observed trend of NWOCI and the light blue region represents the 80% confidence interval for the forecast uncertainty. Also, the scatter points represent the historical values in the training data (2013–2017).
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Figure 9. Forecast components (trend and seasonality) from Prophet-BU model for Middlesex county in MA. N.B: The top panel shows the forecast trend while the bottom panel shows the decomposed yearly seasonal pattern.
Figure 9. Forecast components (trend and seasonality) from Prophet-BU model for Middlesex county in MA. N.B: The top panel shows the forecast trend while the bottom panel shows the decomposed yearly seasonal pattern.
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Figure 10. Bar chart showing the causes of NWO in MA based on outage data from 2013–2018 [21].
Figure 10. Bar chart showing the causes of NWO in MA based on outage data from 2013–2018 [21].
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Table 1. Comparison of Extreme Weather outages (EWO) and Non-Extreme Weather outages (NWO) in MA based on the outage data from 2013–2018. Source: statistics are based on data obtained from MA department of public utilities [21].
Table 1. Comparison of Extreme Weather outages (EWO) and Non-Extreme Weather outages (NWO) in MA based on the outage data from 2013–2018. Source: statistics are based on data obtained from MA department of public utilities [21].
EWONWO
Average Number of Customers Affected144127
Median Number of Customers Affected1413
Average Outage Duration (Hours)13.606.85
Median Outage Duration (Hours)3.571.78
Total Number of Outages61,17375,671
Total Duration of Outages (Days)834,513518,644
Total Number of Customers Affected8,810,0399,680,001
Table 2. Wind threat threshold as defined by NOAA. Source: Adapted from NOAA [46].
Table 2. Wind threat threshold as defined by NOAA. Source: Adapted from NOAA [46].
Threat LevelDescriptionWind Speed (mph)
ExtremeDamaging high wind:
An Extreme Threat to Life and Property from High Wind.
>58
HighHigh wind:
A High Threat to Life and Property from High Wind.
40–57
ModerateVery windy:
A Moderate Threat to Life and Property from High Wind.
26–39
LowBreezy to windy:
A Very Low Threat to Life and Property from High Wind.
21–25
Very lowBreezy:
No Discernable Threat to Life and Property from High Wind.
-
Table 3. Performance comparison of proposed Prophet-TPE model (state level) with other Prophet and SARIMA Bayesian optimized forecasting models.
Table 3. Performance comparison of proposed Prophet-TPE model (state level) with other Prophet and SARIMA Bayesian optimized forecasting models.
RMSE
Prophet-TPE (Proposed Model)18.21
Prophet-Anneal18.59
SARIMA-TPE25.64
SARIMA-Anneal22.25
Table 4. Performance comparison of proposed Prophet-BU hierarchical model (county level) with other Prophet and SARIMA hierarchical forecasting models.
Table 4. Performance comparison of proposed Prophet-BU hierarchical model (county level) with other Prophet and SARIMA hierarchical forecasting models.
RMSE
Prophet-BU (Proposed Model)2.40
Prophet-PHA2.55
Prophet-AHP2.57
Prophet-WLSS2.43
Prophet-OLS2.47
Prophet-WLSV2.59
Prophet-FP3.81
SARIMA-PHA3.80
SARIMA-AHP3.80
SARIMA-WLSS3.80
SARIMA-BU3.81
SARIMA-OLS3.84
SARIMA-WLSV3.81
SARIMA-FP3.81
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Owolabi, O.O.; Sunter, D.A. Bayesian Optimization and Hierarchical Forecasting of Non-Weather-Related Electric Power Outages. Energies 2022, 15, 1958. https://doi.org/10.3390/en15061958

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Owolabi OO, Sunter DA. Bayesian Optimization and Hierarchical Forecasting of Non-Weather-Related Electric Power Outages. Energies. 2022; 15(6):1958. https://doi.org/10.3390/en15061958

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Owolabi, Olukunle O., and Deborah A. Sunter. 2022. "Bayesian Optimization and Hierarchical Forecasting of Non-Weather-Related Electric Power Outages" Energies 15, no. 6: 1958. https://doi.org/10.3390/en15061958

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