Moving Beyond Means: The Outsized Effect of Climate Change on Extremes in Temperature, Load, and Power Markets

Introduction

Any business that makes money from the ERCOT power market knows that not all price hours are equally important. Over the past 5 years, for example, the top 1% of price hours have accounted for an average of 34.4% of the annual spot energy market value (Table 1).

Share of Annual Market Value
from Top 1% Price Hours,
ERCOT North Hub RT
201935%
202017%
202160%
202220%
202340%
Table 1. The share of annual ERCOT North Hub RT value accrued by the highest 1% of hours

Energy prices are heavily skewed and volatile, driven by net load volatility resulting from combinations of high heating/cooling demand and simultaneous low renewables generation (Figure 1). Properly accounting for extremes, in other words, is essential for survival in a rapidly changing market.

Figure 1. Daily average ERCOT North Hub RT prices in 2023

A primary driver of the changing power market landscape, of course, is climate change. Unfortunately, most power market participants rely on unadjusted historical weather data to estimate future market risk (a practice founded on the hidden assumption that the future is like the past) and don’t account for changes in underlying weather distributions over time.

In this blog post, we demonstrate the outsized effect that a shift in weather distributions due to climate change has on the frequency of extremes in both temperature and total system load.

Climate Change and the Expectation of Extremes

Climate change trends are usually studied and reported as expected differences in average magnitudes over a period of time. For example, analysis of historical temperatures across Texas yields a trend of approximately +0.5°F per decade over all of Texas, consistent with CMIP6 climate models. In reality, however, these trends are better understood as shifting entire temperature probability distributions to the right–and not just the resulting shifts in aggregate measures like means and medians (Figure 2). As the probability of an extreme can be understood as the area under the distribution to the right of a particular point, we see from Figure 2 that a shift in distributions has a particularly dramatic effect in the relative frequency of extremes.

Figure 2. Hypothetical distribution of current and new climate under climate change. Source: EPA.gov

Changing Extreme Expectations in ERCOT

To illustrate the outsized effect of climate change on the frequency extreme occurrences of temperature and load in ERCOT, we simulated 1,000 probabilistic hourly weather outcomes for 2024 under two conditions: 1) using unadjusted historical weather data from 1950-present, and 2) applying climate change trends to adjust historical data to current climate conditions. Figure 3 presents the increased occurrence of temperature extremes (population-weighted 100°F+ hours) and load extremes (80 GW+ of RTO load) during all summer hours when accounting for climate change.

The temperature heatmap (top) is fairly straightforward–the effect of increased extreme frequency due to climate change is greatest in early August (when ERCOT temperatures are highest) and centered around the hours beginning 15, 16, and 17 (local time). After accounting for climate trends, 100°F+ hours occur 80 more times over 1000 simulations in the early August late afternoon period, which equates to an 8% increase in the overall likelihood in each hour. 

The load heatmap is more interesting. First, one notes a semi-regular pattern due to decreased load during weekends and holidays. More importantly, however, one finds that the effect of climate change on the frequency of extremes is shifted by about a week or two. Even though extreme temperatures might be more frequent around August 1, extreme load is more frequent around August 7–due to the natural seasonality of cooling demand intensity in Texas. Finally, the heatmap values are significantly different. Accounting for climate trends leads to an additional 300 occurrences of 80 GW load hours during the early August, late afternoon period, or a 30% increase in overall likelihood in those hours.

Figure 3. Climate change effect on extremes in ERCOT. 

Turning to the more relevant market risk metric of relative extreme event frequency increases, we compare the outright likelihood of events in the climate-aware simulations and the unadjusted simulations. Figure 4 presents the outright likelihoods of 80+ GW load in hour beginning 19 in terms of their occurrences per 1,000 climate simulations. In August, extreme load occurs in approximately 5% of simulations that don’t incorporate climate trends, but almost 25% of simulations that do. That’s an over 6x increase in odds of having extreme (80 GW) load (1/19 vs 1/3).  

Figure 4. Occurrences of extreme load hours in ERCOT

Conclusions

Stay tuned for future discussion of the climate change effects on net load!

Case Study: Net demand simulation

This case study presents the underlying motivation and representative insights from an electric cooperative net demand planning exercise that utilized a long-term (15-year) correlated climate simulation and machine learning-based energy resource modeling. The approach described here overcomes several challenges related to net demand planning and resource adequacy analysis, namely– 1) the creation of a large sample of properly jointly distributed weather, 2) the incorporation of climate change trends, 3) the creation of a typical hourly net demand path, and 4) the creation (and curation) of extreme–but realistic–weather and energy scenarios across a utility footprint.

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Case Study: Reduce annual revenue risk by 24%

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Leeward Renewable Energy used the Sunairio platform to select new wind and solar projects that best diversified risks across different regions and different technologies. Sunairio enabled Leeward to simulate thousands of correlated future production and revenue outcomes at dozens of current and prospective sites. The Sunairio platform applied modern portfolio theory to pick an optimal combination of new projects.

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