Parched Power Plants: The Role of Markets and Technology in Power Plants’ Drought Responses

Executive Summary

  • Using water more efficiently in droughts: This paper shows that during droughts market plants in certain regions experience generation reallocation toward less water-intensive, cheaper natural gas-fired plants and away from more costly, water-intensive coal-fired plants. 
  • Adapting to water scarcity by using less water: The authors show that electrical grid operators adjust to droughts by calling on power plants that are 1) less affected, and 2) use less water. This response to drought illustrates the role of technological innovation and operational adjustments in mitigating environmental risks.
  • Managing climate change with market systems: Climate change is likely to create more shortages. This study shows that market-based systems effectively respond to climate change by adjusting the use of scarce resources. The paper contributes to our understanding of how competitive electricity markets can serve as a tool for climate change adaptation, highlighting the importance of market structures in the broader context of environmental and energy policy. Policymakers should strive to understand the role of markets in decarbonization efforts and the value of market-based rules and systems in managing climate change.

1 Introduction

Climate change continues to have wide-ranging effects on the environment and society, often affecting how the two interact. Most policies have addressed climate change through decarbonization efforts in high-emission sectors such as transportation and electricity, particularly as extreme weather events have increased in frequency and stressed the electricity grid (US EPA, 2023a; Tyran, 2023). The electricity sector is especially vulnerable to climatic shocks that climate change can amplify,1Recent examples include the Texas cold snap of February 2021 (which may have been worsened by climate change (Henson, 2021; https://www.washingtonpost.com/weather/2021/09/03/climate-change-arctic-texas-cold/)), Winter Storm Elliott causing generation outages in PJM, drought concerns in ERCOT and SPP (Patel, 2022; https://www.powermag.com//nerc-warns-of-mounting-reliability-risks-urges-preparation-for-challenging-summer/?oly_enc_id=7532C2740301C4R) and the entire Western United States during summer 2022 (Simon, 2022; https://www.npr.org/2022/08/26/1118719636/drought-threatens-coal-plant-operations-and-electricity-across-the-west), and record-setting heat in California in Texas during summer 2023 (Reuters, 2023; https://www.reuters.com/business/energy/us-power-grids-vulnerable-extreme-heat-conditions-this-summer-nerc-2023-05-17/). particularly drought. This is because thermoelectric power plants (which still produce the majority of electricity in the United States, around 60 percent in 2021 (US EIA, 2022)) rely on water for their cooling systems.2Thermoelectric power plants require water to cool their generators’ steam back into a liquid state for reuse in the electricity generation process. In effect, droughts diminish water quantity and quality, thereby decreasing plants’ efficiency and increasing their marginal cost of generation (Putman and Harpster, 2000; Lakovic et al., 2010; Pattanayak, Padhi, and Kodamasingh, 2019).

Competitive (or deregulated) wholesale power markets should efficiently reallocate generation and provide incentives for plants to adapt to drought’s exogenous efficiency and cost shocks. However, does this happen in practice? That is, do power plants located in competitive wholesale power markets experience generation reallocation and adapt to drought as competitive theory predicts? Do plants that are instead located in areas serviced by vertically integrated monopoly utilities, where no competition exists, respond oppositely by bearing the efficiency loss and marginal cost increase? And how do plants’ responses to their own drought state vary with the extent of drought in their operating area? In this paper, we leverage the heterogeneity in electricity market structure across the contiguous United States and exogenous drought shocks to estimate the effect of drought on plant-level efficiency and generation in different markets and market-level drought conditions.3We classify the seven regional transmission organizations (RTOs) and independent system operators (ISOs) in the United States to be our market areas. The remaining nonmarket balancing authority areas are grouped into several regions that represent our nonmarket areas. See Section 2.2 for details.,4Unless otherwise specified, “plant level” hereafter denotes a set of at least one generating unit (e.g., all coal-fired steam turbine generating units or natural-gas-fired combined-cycle generating units at a generating facility). “Plant” alone refers to an entire facility.

We contribute to the literature within the energy-water nexus in ways that highlight the close relationship between energy and water resources. First, we use high-resolution satellite-derived data on the PDSI5The raw data can be found at the University of California Merced Climatology Lab’s PDSI website: https://www.climatologylab.org/gridmet.html. that enables us to obtain plant-level measures of drought conditions over time. These data allow us to construct more precise estimates of local or plant-level drought conditions than coarser measures (e.g., climate-region-level PDSI) used in prior work (e.g., Eyer and Wichman, 2018). Second, we shed light on the efficacy of competitive electricity markets for achieving cost-minimizing generation reallocation across thermoelectric power plants. Such insight is key for informing the management of remaining thermoelectric plants during the decarbonization of the electricity sector.

Third, we provide the first evidence of plant-level efficiency responses to drought using two-way fixed effects regression models. Efficiency adjustments have been shown to be a viable mechanism for responding to cost shocks such as fuel price changes (Doyle and Fell, 2018) and even water temperature changes (Henry and Pratson, 2016), which are a symptom of drought. This evidence augments previous work analyzing plant-level generation responses to drought (Eyer and Wichman, 2018; Mamkhezri and Torell, 2022; Qiu et al., 2023). Finally, we extend previous research’s analyses of plant responses by allowing them to vary based on the extent of drought in a plant’s market (market-drought). This allows us to estimate drought’s effects on plant responses through two avenues: a plant’s own-drought state (which affects their own efficiency and marginal cost) and market-drought (which affects a plant’s responses by altering the market-level electricity supply curve, potentially changing the incentives a plant faces).6In short, a profit-maximizing plant in drought should be incentivized to offset its marginal cost increase (by improving its efficiency or changing its output) only if no or some small proportion of other plants in its market are also in drought. In the extreme case where a plant’s entire market is in drought, then the supply curve essentially remains unchanged (merely shifted up) and any individual plant has no incentive to adjust its efficiency or generation. See Section 3 for details.

Our results broadly show that wholesale electricity markets work as intended for reallocating generation from water-intensive to less water-intensive plants during drought (i.e., shifting generation toward less water-intensive and lower-cost natural-gas-fired plants). For capacity factor (a measure of plant usage), combined-cycle natural-gas-fired market plants experience increased capacity factor during drought as their market allocates more generation to them. However, we also find some regions’ nonmarket plants experiencing the same capacity factor effects as their market counterparts, indicating that nonmarket entities find mimicking market outcomes to be advantageous. We also find that the capacity factor of market coal-fired plants decreases during drought, albeit only in Texas during drought-intensive years, lending some credence to the importance of drought persistence and frequency. For heat rate (a measure of plant efficiency), we chiefly find that only market peaker plants using simple-cycle steam generators decrease their heat rate (improve their efficiency) during drought as expected.

Our analyses of market-drought’s effects mostly find that market plants experience higher capacity factors when they are not in drought but more of their market is. Conversely, they experience lower capacity factors when they are in drought and less of their market is affected by it. However, we find very little evidence of market-drought affecting market plants’ heat rate. The capacity factor effects are in line with our theoretical expectations for market-drought that are based on wholesale electricity markets’ use of a merit order to construct a supply curve that orders plant offers from least to greatest cost. When a market plant is not in drought but more of their market is, the plant will be called upon to generate more often since their costs are not increased by drought, unlike the rest of the market. Conversely, when a market plant is in drought and less of their market is, then less of the market’s supply curve is reordered due to increased costs while the plant is shifted out. This shift reduces the generation that the plant is called upon to provide.

Shedding light on plant-level efficiency and generation responses to drought is important for better understanding the role of markets in the water-energy nexus amid decarbonization efforts and a growth in reliability concerns as extreme weather events occur more frequently. The transition to a decarbonized energy sector will not happen overnight, so society must contend with the existing fleet of fossil fuel plants and its adaptation to climate change until renewable energy sources comprise most of the generation fleet. The crux of this paper is the difference in adaptation incentives and responses across market types (i.e., between competitive markets and vertically integrated monopolies), whether such a difference ultimately brings about favorable changes in plant operations, and how the extent of drought in a market affects its salience. Plants operating in market (deregulated) areas face incentives to remain cost-competitive and mitigate or fully offset drought’s effects on their marginal cost through efficiency improvements7Efficiency improvements can be made by decreasing heat rate, which is defined as the amount of fuel combusted divided by the amount of electricity generated. Examples of heat rate adjustments include improving steam trap management, improving the performance of feedwater chain systems, improving the maintenance of generators’ air filtration units, and controlling boiler flue gas oxygen content (Hite, 2013; Doran, 1997; Hunt, 2007; Maize, 2018; Kambaladinne, 2015; McClintock, 2018a). or market-enacted changes to their generation, while plants operating in nonmarket (regulated) areas are cogs in their respective utility’s monopoly machine and face no such incentives. By virtue of being regulated, utilities operating plants in nonmarket areas are not allowed to earn profit on maintenance or fuel costs, which both affect plant efficiency; these are operating expenses that utilities are not allowed to mark up (Kibbey, 2021).8Utilities are guaranteed a rate of return on capital expenses or investments such as substations, power plants, and power lines (Feinstein and de Place, 2020). These plants (and the utilities that operate them) then have little to no market incentives to improve their efficiency or change their generation. Thus, large swaths of the United States have their electricity needs serviced by entities that may be relatively unresponsive to climate change’s effects.9Since they are allowed to earn a rate of return on capital investments, utilities in regulated or nonmarket cost-of-service areas would prefer to make a discrete change to renewables once their costs are low enough rather than progressively decarbonizing their generation by improving efficiency and thus reduce their fossil fuel consumption. As for competitive markets, it remains to be empirically verified if competitive incentives actually work as intended in the context of climate-change-induced cost/efficiency shocks such as drought.10Doyle and Fell (2018) show that natural gas plants respond to changes in fuel costs along both the generation and efficiency dimensions. If competitive markets work as intended, then they could be a viable method of shifting electricity generation toward less costly plants and incentivizing improved plant efficiency, enabling emissions reductions and cost savings in the face of climate change.

Previous work has largely focused on either the market-level effects of drought on generation, capacity, or electricity prices (van Vliet, Vögele, and Rübbelke, 2013; McDermott and Nilsen, 2014; Pechan and Eisenack, 2014; Kern and Characklis, 2017; Byers et al., 2020; Fonseca et al., 2021) or on the firm-level effects of drought on financial outcomes or investment behavior (Kern and Characklis, 2017; Bogmans, Dijkema, and van Vliet, 2017). Ganguli, Kumar, and Ganguly (2017) and Chandel, Pratson, and Jackson (2011) diverge from most of the literature by examining national-scale generation effects of drought and policy’s effects on power plant water usage, respectively. Moreover, many existing studies employ simulations rather than econometric models like the ones we use in this paper (van Vliet, Vögele, and Rübbelke, 2013; van Vliet et al., 2016). The papers that are most similar to ours are Eyer and Wichman (2018) and Golombek, Kittelsen, and Haddeland (2011). However, Eyer and Wichman focus only on generation effects using a coarser drought measure (climate-region-level PDSI), and Golombek, Kittelsen, and Haddeland use a simulated market-level model to identify efficiency effects. We use a much finer drought measure and provide plant-level analyses of efficiency and generation responses.

The rest of this paper proceeds as follows. Section 2 provides essential information on the relationship between thermoelectric power plants and drought and on US wholesale electricity markets. Section 3 elucidates our conceptual model of market versus nonmarket plant drought responses and theoretical model of plant efficiency and generation responses to market-drought from a competitive, profit-maximization perspective. Section 4 describes the data used for estimating our econometric models, which are detailed in Section 5. Section 6 reports the results of estimating our econometric models of plant responses. Section 7 discusses the results’ general and policy implications as well as avenues through which unanticipated results may have formed. Section 8 concludes.

2 Background and Industrial Setting

2.1 Thermoelectric Power Plant Water Usage and Drought

Thermoelectric power plants are plants that use steam turbine or combined-cycle generating units.11Combined-cycle plants use both a gas and steam turbine in tandem to generate up to 50 percent more electricity from the same amount of fuel than conventional simple-cycle (single turbine) plants (GE Gas Power, n.d.). The gas turbine burns fuel to generate electricity, and its exhaust heat is captured and used in the steam turbine to run its steam-powered turbine. Such plants require water to cool their generators’ steam back into liquid form for reuse in their power generation process. Plants extract cooling water from surface waters (e.g., lakes, rivers, and streams) and feed it into a condenser, where used steam exiting the turbine enters and is cooled (condensed) back into liquid form. The extracted cooling water, having absorbed the steam’s heat, is then discharged directly back to its source (in once-through cooling systems) or to a cooling tower/pond (in recirculating cooling systems).12Once-through and recirculating cooling systems are the most prevalent, but dry and hybrid cooling
technologies also exist and are used for about 3 percent of US thermoelectric capacity (US EIA, 2018).
The cooled steam water is then pumped back to the boiler to be heated into steam again. The steam proceeds to turn the blades of the turbine and the rotor shaft of the generator before reentering the condenser to repeat the process all over again. Figure 1 provides a graphical illustration of thermoelectric plants’ water usage process (for those with once-through cooling systems).13See Appendix A for details on this process and drought’s effects on plant efficiency and marginal cost. Note that the process entails differing levels and rates of water withdrawal and consumption14On average, 96 percent of water gets returned to its source once generator steam has been cooled (Northern Great Plains Water Consortium, 2022). across cooling system types, namely once-through, recirculating, dry, and hybrid.15Due to incomplete information on plants’ cooling systems at the national level, we do not exploit heterogeneity in cooling system types in our analyses; Mamkhezri and Torell (2022) are able to do so in their analysis of drought’s effects on emissions and generation but only in Texas. See Appendix E for more information on different cooling system types.

Figure 1. Basic Illustration of How Water Is Used at Thermoelectric Power Plants

Notes: Figure source is Reimers (2018)

Drought is generally defined to be precipitation deficiency over an extended time period (e.g., a month). The American Meteorological Society goes a step further and defines it as “a period of abnormally dry weather sufficiently long enough to cause a serious hydrological imbalance” (Drought.gov, n.d.). For the purposes of this paper, we focus specifically on hydrological drought as it is most salient to power plant operations.16The other types of drought are meteorological drought, agricultural drought, socioeconomic drought, and ecological drought. Hydrological drought is prolonged precipitation deficiency in surface (e.g., lakes, rivers, and streams) or subsurface (e.g., groundwater) water supply (National Drought Mitigation Center, 2022). That is, it concerns the lack of water in the hydrological system that manifests in the form of unusually low river streamflow and unusually low levels of water in other surface waters and groundwater (Van Loon, 2015).

Low streamflows are a direct consequence of drought, and high water temperatures are a symptom that typically accompanies drought (Kimmell and Veil, 2009). Thermoelectric power plants are generally vulnerable to low streamflows, high ambient air temperatures, and high water temperatures (Bartos and Chester, 2015).17Plants using once-through cooling systems are affected by low streamflow and high water temperatures, while those using recirculating cooling systems are affected by those same factors in addition to high air temperature (Bartos and Chester, 2015). Thus, regardless of a generating unit’s prime mover or a plant’s cooling system, drought essentially imparts two effects upon plants: an increase in the marginal cost of generation and a decrease in generating capacity (or derating). The marginal cost effect is our main channel of interest, and it results from drought increasing intake water temperature or decreasing available water levels.

Previous research has established that both higher intake water temperatures and lower streamflow negatively affect plants’ generating capacity (van Vliet et al., 2012; Bartos and Chester, 2015) and efficiency (Stillwell, Clayton, and Webber, 2011; Zammit, 2012; Colman, 2013; Denooyer, 2015; McCall, MacKnick, and Hillman, 2016; Petrakopoulou, 2021). In this paper, we measure efficiency with a plant’s heat rate HR, defined as

    \[H R=\frac{\text { Fuel combusted (MMBtus) }}{\text { Electricity generated (MWhs) }}\]

In short, lower efficiency (higher heat rate) results from higher condenser pressure; the engineering literature has shown that both higher intake water temperatures and lower streamflow increase condenser pressure (Putman and Harpster, 2000; Pattanayak, Padhi, and Kodamasingh, 2019). Higher pressure within a plant’s condenser (where steam is cooled back into liquid form) is associated with lower turbine efficiency for both single-cycle steam turbines and the steam engine component of combined-cycle turbines. This is because an increase in condenser pressure causes a turbine’s endpoint enthalpy to increase, leading to a loss in generation.

Higher steam flow is then needed to maintain the prior level of generation, and this higher steam flow is achieved by increasing the turbine’s throttle and combusting more fuel (Putman and Harpster, 2000; Lakovic et al., 2010; Pattanayak, Padhi, and Kodamasingh, 2019). This increased fuel combustion to produce the same amount of electricity is the source of lessened efficiency. Lakovic et al. (2010), Zammit (2012), Denooyer (2015), and Pattanayak, Padhi, and Kodamasingh (2019) all show that higher cooling water temperature leads to higher condenser pressure and lower efficiency. McCall, MacKnick, and Hillman (2016), Pattanayak, Padhi, and Kodamasingh (2019), and Petrakopoulou (2021) show that a lower cooling water flow rate or water availability increases condenser pressure and lowers efficiency overall. See Appendix A for a more detailed exposition of how drought affects condenser pressure and, ultimately, plant efficiency.

2.2 US Wholesale Electricity Markets

In this paper, we focus on markets for wholesale electricity generation (i.e., not retail markets that sell power to end users such as households) since these are the markets that power plants operate and face external cost shocks (e.g., drought). The United States is home to two types of wholesale electricity markets: competitive markets (located in deregulated regions) and vertically integrated monopolies (located in the regulated utilities’ service territories).

Figure 2 illustrates the spatial distribution of US wholesale electricity markets and how we classify market and nonmarket plants. We designate the seven regions governed by the seven RTOs and ISOs as our market areas since they operate competitive wholesale electricity markets. Consequently, we classify all plants operating in these RTOs/ISOs as market plants. These RTOs/ISOs are the California Independent System Operator (CAISO), Electric Reliability Council of Texas (ERCOT), Southwest Power Pool (SPP), Midcontinent Independent System Operator (MISO), PJM Interconnection (PJM), New York Independent System Operator (NYISO), and ISO New England (ISONE). We designate all of the
balancing authority areas in the gray areas as nonmarket areas, that is, areas serviced by a vertically integrated monopoly utility.18Balancing authority areas are entities that balance generation and load (demand) in their respective service areas (NERC Resources Subcommittee, 2011). The gray areas in Figure 2 are composed of a plethora of balancing authority areas, each with their own service area (see Appendix B and Appendix C for maps of balancing authority areas). Each of the 7 RTOs/ISOs is actually a balancing authority area as well. Including the 7 RTOs/ISOs, there are 66 balancing authority areas in the United States (US EIA, 2016). We classify all plants operating in the gray areas as nonmarket plants19Technically, there are markets for electricity in these areas, but they are monopolies. For the purposes of this paper, we term such monopolies “nonmarket” to highlight that no competitive market exists. In electricity parlance, “market” areas are deregulated regions and “nonmarket” areas are regulated regions. and define two regions to allow for heterogeneous responses based on regional differences in utility operations:20For example, a nonmarket plant in Florida may share a similar or congruent market structure with a nonmarket plant in Arizona, but each operates in distinct natural and societal environments. West (which includes all balancing authorities in the Western Interconnection besides CAISO21The US electric grid is split into three regions: the Eastern Interconnection (composed of states east of the Rocky Mountains), the Western Interconnection (composed of states west of the Rocky Mountains), and Texas (US EPA, 2023b).,22See Appendix C for a map of Western Interconnection balancing authority areas.) and Southeast (which is effectively captured by the SERC Reliability Corporation’s regional footprint).23The SERC Reliability Corporation ensures reliable electricity access for Alabama, Florida, Georgia, Mississippi, Missouri, North Carolina, South Carolina, and Tennessee and parts of Arkansas, Illinois, Kentucky, Louisiana, Oklahoma, Texas, and Virginia. The nonmarket balancing authority areas within these regions are serviced by a single vertically integrated monopolist utility that owns and operates generation, transmission, and distribution resources.

Figure 2. Map of US RTOs

Notes: Figure source is Sustainable FERC Project (2020).

Our analyses are carried out in several configurations: full sample, Western Interconnection, Eastern Interconnection, Texas, and individual RTOs/ISOs (see Section 5 for details on these configurations). Some states in our nonmarket regions overlap with states that are part of our market areas or RTOs/ISOs, but we classify plants based on whether they are in an RTO/ISO or not even if they are located in a state that is partially part of an RTO/ISO and a nonmarket area. For example, CAISO includes the state of California, but California also contains some plants that are part of the Balancing Authority of Northern California (BANC). Plants that operate within CAISO are classified as market plants, and those that operate as part of BANC are classified as nonmarket plants.

Competitive wholesale electricity markets separate the market for electricity generation from electricity transmission and distribution. The demand side of these markets typically consists of electric utilities and nonutility power providers,24If a region offers retail choice for electricity to its consumers. while the supply side consists of independent power producers and electric utilities. These markets generally operate as follows.25There are actually two types of wholesale markets: the day-ahead market and the real-time market. The description of wholesale market operations is mostly relevant to the day-ahead market, wherein RTOs/ISOs clear the market for the next day a day in advance. Real-time markets operate similarly, but rather than allocate supply for predicted load, they clear the market for real-time electricity imbalances (i.e., shortages and exceedances) at high frequencies of every 15 or even 5 minutes. All RTOs/ISOs have both types of markets. The RTO/ISO first determines how much electricity demand (or load) there is or will be to serve. Electricity suppliers submit bid prices (equal to their marginal cost of generation) for the amount of electricity that they choose to supply. The RTO/ISO then performs a process called economic dispatch to order suppliers (plants) by marginal cost (ascending from lowest cost to highest cost) and construct the electricity supply curve.

The final ordering is called the merit order. Moving down the merit order is equivalent to moving to the left in the ordering (and supply curve), while moving up is equivalent to moving to the right in the ordering (and supply curve). The result is a discontinuous step function for the electricity supply curve,26See Appendix D for an example of a supply or dispatch curve. where the market-clearing price received by all suppliers is the marginal cost of the market-clearing or marginal supplier (i.e., the last supplier called upon to fulfill load).27Suppliers with marginal costs below the market-clearing price are inframarginal suppliers that earn per-unit inframarginal rents equal to the difference between the market-clearing price and their marginal cost. The marginal supplier earns no such rents by virtue of being the price setter (such that the price they receive is exactly equal to their marginal cost). Changes to marginal cost due to exogenous factors like drought naturally affect plants’ position on the supply curve and, consequently, whether they are inframarginal, marginal, or not called upon to generate at all. Increased marginal cost moves a plant up (or to the right) the merit order and supply curve, while decreased marginal cost moves a plant down (or to the left) the merit order and supply curve.

Operations in regulated or nonmarket areas serviced by vertically integrated monopoly utilities look much different than competitive wholesale markets. Like RTOs, these utilities also determine how much load to serve and operate economic dispatch of their plants. But that is where the similarities end. Utilities mainly serve load using their own plants according to their own decisions regarding plant dispatch, but they can also engage in bilateral electricity trading with other utilities.28Regulated utilities are increasingly participating in real-time energy imbalance markets, where they transact shortages or exceedances with other utilities or competitive suppliers; see the Western Energy Imbalance Market (whose website is https://www.westerneim.com/Pages/About/default.aspx) or the nascent Southeast Energy Exchange Market (whose website is https://southeastenergymarket.com/). However, these transactions comprise a very small percentage of utilities’ total supply, and so we do not consider them in this paper. The electricity prices faced by end users such as households are fixed by regulation that is typically performed by state utilities commissions; no wholesale electricity price arises because there is no competition in generation. By law, these utilities are guaranteed a predetermined rate of return on capital investments or expenses, but they are not allowed to earn any profit on operating expenses such as fuel or maintenance costs. This type of regulation incentivizes investment in infrastructure (e.g., new power lines, generators, and entire plants) over improving existing technologies or operations (e.g., improving efficiency or reducing maintenance costs) since the latter amounts to increasing operating expenses that utilities cannot earn profit on.

3 A Conceptual and Theoretical Framework for Power Plant Drought Responses

In this section, we motivate our empirical analyses with a conceptual and theoretical exposition of plant behavior in and out of drought. We first elucidate our conceptual framework for differing drought responses between market and nonmarket plants. This framework allows us to ground our econometric models in market structure theory and define our market versus nonmarket hypotheses. We then cast market plants’ drought responses as the solution of a competitive profit-maximization problem that introduces drought as an exogenous variable in plants’ marginal cost and hours in operation functions. This approach enables us to derive comparative statics and hypotheses that we test empirically using the data described in Section 4 and econometric framework detailed in Section 5.

As Section 3.3 describes in more detail, our profit-maximization model takes the perspective of a plant operating in a competitive wholesale market (i.e., a market plant), which implies that we expect nonmarket plants to respond differently or ambiguously (possibly due to unobserved private operating factors) or not respond at all to market-drought (i.e., that market-drought does not enter their objective function). Given the lack of competition in nonmarket regions, the most salient drought factor for nonmarket plants should be their own drought condition, hence our focus on the responses of market plants to market-drought.

Although market plants’ only choice variable in our theoretical model is their change in heat rate, our econometric framework tests drought’s effects on plants’ heat rate and capacity factor. This is because we assume that plants produce as much as they can whenever they are called upon to produce even if they are derated by drought. Any changes (reductions) in capacity factor are due to drought increasing marginal cost, which thereby affects whether a plant is inframarginal, marginal, or not called upon and, consequently, their capacity factor. Thus, our empirical results for capacity factor effects are a result of marginal cost changes and not necessarily plants choosing different generation levels.

Our conceptual and theoretical models assume that drought is sufficiently salient to plants so as to influence them to respond. Given climate change’s growing impacts on weather events, this seems like a reasonable assumption to make. However, it is possible that drought frequency and persistence affect whether or not plants respond to drought at all;29If drought is a relatively rare event or if it does not last for very long, then plants may prefer to continue operating under business-as-usual practices rather than respond to drought. That is, the costs of operating normally in drought (i.e., with higher marginal cost and lower efficiency) are lower than the costs of adjusting heat rate or bidding at higher marginal cost such that capacity factor is reduced. in the context of this paper, persistence refers to drought duration, and frequency refers to how often drought events occur (not necessarily consecutively). This is a possibility that we explore in our empirical analyses by studying plant responses during temporal subsets in which drought was frequent or persistent (by market area).

Finally, our theoretical model posits an undefined planning horizon for plant decisions. This allows us to derive comparative statics for situations where plants’ planning horizons coincide with drought frequency. However, it also reflects that we do not know what plants’ planning horizons are with respect to heat rate or capacity factor changes specifically in response to drought. Our empirical analyses implicitly assume a monthly planning horizon due to our monthly data on plant generation and heat rate, but it is possible that plants respond to drought according to longer or shorter periods.

3.1 Market versus Nonmarket Plants’ Own-Drought Responses

We define own-drought to be an individual plant’s drought condition (e.g., in drought; not in drought; mild, moderate, or severe drought). Drought reduces the quantity of water available (the quantity effect) and increases water temperature (the temperature or quality effect). Through these two effects, drought ultimately imparts the following effects upon plant operations:

  • reduced generating capacity (or derating), caused by drought’s quantity effect
  • increased marginal cost, caused by drought’s quantity and quality effect

We now briefly describe the pathways drought takes to impart these effects on capacity and marginal cost, beginning with capacity (specifically capacity factor):30Capacity factor is a generating unit’s actual output divided by its maximum generating capacity.

  1. Drought’s quantity effect causes the water level to decrease, diminishing the plant’s water supply.
  2. Plants become capacity constrained (or derated); that is, their maximum output is reduced due to the decreased water supply.
  3. Plants’ output is reduced below what it would have been absent drought conditions,31In the context of this study’s empirical framework, plants reduce their month-level output and capacity factor, where both generation and maximum capacity have been aggregated to the monthly level. decreasing capacity factor.

Keeping with drought’s quantity effect, we now turn our attention to marginal cost:

  1. Drought’s quantity effect causes the water level to decrease, diminishing the plant’s water supply.
  2. Water’s mass flow rate into condensers decreases (Petrakopoulou, 2021).
  3. Heat rate increases (efficiency decreases).
  4. Reduced efficiency increases the per unit of electricity expenditure on fuel32Drought can also increase per unit of electricity fuel expenditure if fuel demand from fossil fuel plants increases (either to make up for lost hydropower generation under drought or to service increased electricity demand during drought). such that more fuel is needed to produce the same amount of electricity → marginal cost increases.

Finally, marginal cost is also affected by drought’s quality effect:

  1. Drought’s quality effect increases water temperature.
  2. Plants’ intake water temperatures increase.
  3. Heat rate increases (efficiency decreases).
  4. Reduced efficiency increases the per unit of electricity expenditure on fuel such that more fuel is needed to produce the same amount of electricity → marginal cost increases.

These capacity factor and marginal cost effects would manifest if plants did not respond to drought at all (i.e., if they did not adjust their efficiency or if their capacity factor was not changed by supply curve changes due to drought). In reality, market plants face private and market incentives to adjust their efficiency and will likely experience changes to their capacity factor based on realized drought conditions. On the other hand, nonmarket plants do not face such market incentives to remain cost-competitive and instead have the option of passing on increased costs due to drought to consumers. In addition, their operating utilities/entities do not have access to a centralized wholesale electricity market and instead must rely on bilateral trading with other utilities/entities. Thus, we expect differing drought responses between market and nonmarket plants.

With respect to capacity factor effects, because drought increases plants’ marginal cost of generation, market areas should reallocate generation from water-intensive plants (that experience the greatest cost increases due to drought) to less water-intensive plants (that experience smaller cost increases than water-intensive plants) to meet demand at least cost. In terms of electricity supply in market areas, this means that plants whose cost increases are shifted right on the supply curve (or merit order), with water-intensive plants being shifted farther to the right than less water-intensive ones. Coal and natural gas are the primary fossil fuels used in thermoelectric plants, and because coal-fired plants use more water than natural-gas-fired plants (Union of Concerned Scientists, 2013; US EIA, 2023a), we classify coal plants as water intensive and natural gas plants as less water intensive.33Coal plants consistently use more water than natural gas plants regardless of cooling system used (Union of Concerned Scientists, 2013). Moreover, in 2021 the US Energy Information Administration (EIA) estimated that coal generation had an average water withdrawal intensity of 19,185 gal/MWh, while natural gas generation had an average water withdrawal intensity of 2,803 gal/MWh (US EIA, 2023a). Even if both gas- and coal-fired plants are in drought, gas-fired plants should experience higher capacity factor as generation is reallocated to them instead of coal-fired plants despite the costs of both plant types increasing. The key here is that gas-fired plants’ costs increased by less than coal-fired plants’ cost increase due to drought. Thus, we expect market plants’ capacity factor to increase in drought if they are natural gas fired and to decrease in drought if they are coal fired.

Nonmarkets do not face the same competitive cost-minimization incentives as market plants, and they must rely on costlier bilateral trading instead of a centralized wholesale market. Therefore, we do not expect the same reallocation from coal to natural gas to occur among nonmarket plants, and instead expect drought to decrease capacity factor for all plant types (through derating). However, there are two scenarios in which nonmarket plants may behave like market plants. First, nonmarket operating entities or utilities may exercise fleet-wide generation reoptimization when drought occurs.34This possibility was pointed out in a helpful reviewer’s comment. Such behavior is possible since a nonmarket utility or entity has control over all plants in its service territory. This behavior would make sense if the reliability benefits of generation reoptimization are large enough. Second, some nonmarket regions may have sufficient access to low-cost bilateral trading to closely mimic wholesale markets.

Heat rate effects in market versus nonmarket plants are more straightforward. Drought should cause heat rate decreases in market plants since they face competitive incentives to reduce their marginal cost and remain cost-competitive during drought. Conversely, nonmarket plants face no such incentives and are also not allowed to earn a return on operating expenses (like improving efficiency by reducing heat rate). Instead, they may prefer to make new capital investments (on which they can earn a regulated return) as opposed to reducing their marginal cost through efficiency improvements that they are not allowed to mark up. Therefore, we expect drought to cause heat rate increases in nonmarket plants as they bear the efficiency loss due to drought.

Our overarching market versus nonmarket hypothesis is therefore the following:

  • H0: Drought increases capacity factor for natural-gas-fired market plants, decreases capacity factor for coal-fired market plants and all nonmarket plants, causes market plants to decrease their heat rate, and causes nonmarket plants to experience increased heat rate.

3.2 Market Plants’ Market-Drought Responses: Mechanisms and Intuition

The own-drought effects (on heat rate and capacity factor) described in Section 3.1 likely depend on the drought condition of the market that they operate in (i.e., market-drought; the extent of drought in a market that we define as the proportion of total thermoelectric capacity that is in drought at some time period).35This logic does not apply to nonmarket monopoly utilities since they are the lone participant in their market and so face no incentive to compete on cost with any other plant or entity. Only own-drought conditions would be relevant for their generation and efficiency responses to drought. Own-drought shifts a plant’s position in its market’s merit order (through its effects on plant marginal cost), and market-drought affects the extent of that shift by affecting the overall change in the market’s merit order or supply curve.36For example, suppose that only one plant in a market is in drought. If the plant is in drought, then it will shift up the merit order and receive less (or zero) profit per unit of electricity or not be called upon to generate at all. However, if more plants in the market are in drought (i.e., more capacity is in drought; market-drought is higher), then more plants are experiencing an increase in marginal cost and more of the supply curve is being shifted up. Thus, the original plant in drought faces less of a displacement in the merit order. The extreme case is that the entire market is in drought (market-drought is equal to one, or all of a market’s capacity is in drought), which would essentially mean that the merit order is unchanged. Thus, for any individual plant i, three principal cases arise:

  1. Case 1: All plants in its market are in drought (i.e., a high proportion of the market’s total capacity is in drought; market-drought is equal to one), including plant i.
    Thus, all plants experience an increase in marginal cost, the entire supply curve shifts up, and the merit order remains unchanged. No plant has an incentive to change their efficiency, and they are called upon to generate with the same probability as without drought (since the entire supply curve is shifted up). Therefore we expect i’s capacity factor to be unchanged or decrease slightly and heat rate to increase (efficiency to decrease).
  2. Case 2: Plant i is in drought, but very few other plants in its market are in drought (i.e., a low proportion of the market’s total capacity is in drought; market-drought is low).
    Plant i experiences an increase in marginal cost and gets shifted up the merit order and supply curve. This increase in marginal cost and consequent higher position on the supply curve cause i to generate less (since it is less likely to be inframarginal) and reduce its heat rate to remain cost-competitive. The plant may also be derated due to drought, which would also reduce its generation by reducing its capacity. Thus, we expect i’s capacity factor to decrease and heat rate to decrease (efficiency to increase) or be unchanged.
  3. Case 3: Plant i is not in drought, but many other plants in its market are (i.e., a high proportion of the market’s total capacity is in drought; market-drought is high).
    Plant i’s marginal cost does not increase, but other plants’ marginal costs do, so they move up on the merit order and supply curve. Consequently, plant i is more likely to be inframarginal, and so its generation (capacity factor) would increase. This case has ambiguous effects on i’s heat rate (drought is not exogenously lowering it, but there are external benefits to further lowering marginal cost, so heat rate may be unchanged or minimally decreased).

Intermediate cases are easily captured by varying own or market-drought.37This is the approach we take for estimating and interpreting our coefficients of interest in our econometric framework. For example, one can travel closer toward case 1 from case 2 by increasing the proportion of a market’s total capacity that is in drought (i.e., increasing market-drought). Moreover, one can switch between case 2 and case 3 by reducing/increasing own-drought.

Finally, note that although the pathways connecting drought to capacity and generation still apply to plants in nonmarket areas, these nonmarket plants do not abide by the logic in the three previous principal cases. This is because such plants are all owned and operated by a single monopoly utility, facing no competition from other plants in their utility’s service area. Thus, only own-drought conditions should be relevant for nonmarket plants’ efficiency and generation responses to drought.

3.3 A Model of Market Plant Profit-Maximization with Drought

We now generalize the plant behavior described in Section 3.2 and explore drought’s effects on plant capacity factor and efficiency using a model of plant-level profit-maximization. Because plants operating in nonmarket areas do not face the competitive incentives discussed in Section 3.2 (by virtue of functioning in a monopoly), we specifically model the profitmaximization performed by competitive plants operating in market areas. The implication of this choice and Section 2.2’s description of vertically integrated monopoly utilities is that nonmarket plants either ambiguously or do not adjust their own-drought responses based on market-drought. This may be due to unobserved operational factors that drive their private decisions or to market-drought not entering their profit-maximizing objectives.

Suppose that in each month, a plant operating in a competitive wholesale electricity market chooses its change in heat rate over a month \Delta H R to maximize its per-month profits. The choice variable follows Doyle and Fell (2018) and is given by \Delta H R=H R_0-H R_1, where H R_0 is a plant’s heat rate before any changes and H R_1 is its chosen (possibly changed) heat rate at the end of a month. With this definition, the choice of a lower heat rate (an efficiency improvement) is represented by choosing \Delta H R>0. Plants can adjust their heat rate in several ways and not only when exogenous shocks like drought occur. Examples of heat rate adjustments include improving steam trap management, improving feedwater chain system performance, improving the maintenance of generators’ air filtration units, enhancing or upgrading unit components,38For example, upgrades to turbine steam seals or installing automated boiler drains (Korellis, 2022). and better managing controllable parameters like boiler flue gas oxygen content.39McClintock (2018b) notes that a “time-tested approach” to managing a plant or generator’s operational efficiency is “monitoring controllable parameters,” which are parameters that are under a unit operator’s control. Examples include boiler flue gas oxygen content, final feedwater temperature, and superheater attemperator sprays.,40See Hite (2013), Doran (1997), Hunt (2007), Maize (2018), Kambaladinne (2015), and McClintock (2018a) for details on adjustment mechanisms for plant heat rates. These adjustments are costly,41Cost estimates for controllable parameter adjustments or maintenance improvements are seemingly not available. However, some cost estimates of more significant technological upgrades/enhancements are available. For example, upgrading a 500 MW plant’s feed pump can cost $600,000 (Lashof et al., 2013). so a rational profit-maximizing firm would only perform such adjustments when the benefits of doing so outweigh the costs.42Experiments have shown that enhancing or replacing unit technology yielded heat rate decreases ranging from 0.1 to 2.5 percent, while improving maintenance of existing unit technologies and parameters yielded heat rate decreases ranging from 0.03 to 1.5 percent (Korellis, 2022). Moreover, Maize (2018) describes a case where an Italian combined-cycle gas-fired plant upgraded its performance modeling technology and experienced an efficiency improvement greater than 1 percent. Moreover, the frequency and consistency of drought may affect whether or not a plant actually adjusts its efficiency at all. It is possible that plants do not respond to infrequent or short-lived drought. While our theoretical model implicitly assumes that drought is sufficiently salient to plants, we test whether plants’ responses depend on drought frequency or consistency in our empirical analyses.

Let own-drought and market-drought be denoted by D_o and D_m, respectively, such that higher values of either correspond to worse drought. Finally, let f denote the per-unit price of fuel. Because drought’s ultimate effect (absent a response by the plant) is an increase in marginal cost, let marginal cost of generation MC be given by

    \[M C=M C\left(f, D_o, \Delta H R\right),\]

with partials \frac{\partial M C}{\partial f}>0, \frac{\partial M C}{\partial D_o}>0, and \frac{\partial M C}{\partial \Delta H R} \leq 0.43Market-drought D_m is not an argument of the MC function because we assume that drought’s effects on other plants in a market do not affect an individual plant’s technology or efficiency. To clarify the plant’s decision-making process in adapting its heat rate (efficiency) to drought, below is the sequence of events faced by all market plants:

  1. Exogenously determined drought states are realized (e.g., no drought, mild drought, severe drought).
  2. Plants observe D_o, D_m, load conditions in their balancing authority area, and how
  3. much their own capacity and heat rate is affected (i.e., H R_0).
  4. Plants choose their change in heat rate \delta H R given their observed (and now fixed) H R_0.

We model the intuition and generalization of the principal cases in Section 3.2 by exploiting the fact that drought affects plants’ position on the supply curve through its effects on MC. This amounts to drought affecting plants’ ability to be an inframarginal or marginal generator and the total number of hours in a month in which a plant has positive generation (either as an inframarginal or marginal generator).44This approach is akin to Doyle and Fell’s (2018) modeling of a plant’s number of hours with positive generation. A plant’s number of hours in a month with positive generation depends on its own-drought and market-drought. Let the number of hours in a month in which a plant has positive generation be given by

    \[H=H\left(f, D_o, D_m, \Delta H R\right),\]

with partials \frac{\partial H}{\partial f} \leq 0, \frac{\partial H}{\partial D_o} \leq 0, \frac{\partial H}{\partial D_m} \geq 0, \frac{\partial H}{\partial \Delta H R} \geq 0.45The effects of own-drought and market-drought can be diminished by each other: \frac{\partial^2 H}{\partial D_o \partial D_m}<0, \frac{\partial^2 H}{\partial D_m \partial D_o}<0. That is, own-drought’s negative effect on H gets smaller as market-drought increases, and market-drought’s positive effect on H gets smaller as own-drought increases.These partials state that an increase in own-drought (worsened own-drought) or fuel price decreases the number of hours in which a plant has positive generation; an increase in market-drought (worsened market-drought) increases the number of hours in which a plant has positive generation; and improving efficiency increases the number of hours in which a plant has positive generation.

Letting the cost of heat rate changes be given by C(\Delta H R) (with C^{\prime}(\cdot)>0) and the
per-unit market price of electricity be p, the plant’s profit-maximization problem is

(1)   \begin{equation*}\underset{\Delta HR}{\text{max}}\;\;\; \pi=\left[p-MC\left(f,D_o,\Delta HR\right)\right]qH\left(f,D_o,D_m,\Delta HR\right)-C\left(\Delta HR\right),\end{equation*}

with first-order condition (omitting functional arguments for brevity)

(2)   \begin{equation*}\displaystyle\frac{\partial\pi}{\partial \Delta HR}=(p-MC)q\frac{\partial H}{\partial\Delta HR}-qH\frac{\partial MC}{\partial\Delta HR}-\frac{dC}{d\Delta HR}=0.\end{equation*}

Differentiating Equation (2) with respect to D_m yields

(3)   \begin{equation*}\frac{\partial^2\pi}{\partial\Delta HR\partial D_m}=(p-MC)q\frac{\partial^2 H}{\partial\Delta HR \partial D_m}-q\frac{\partial MC}{\partial\Delta HR}\frac{\partial H}{\partial D_m}.\end{equation*}

Assuming that \displaystyle\frac{\partial^2 H}{\partial\Delta HR \partial D_m}\geq 0,46This amounts to assuming that an increase in market-drought amplifies \deltaH R‘s positive effect on H. This is plausible for plants that are not in drought since more of the supply curve is disrupted while plants not in drought remain in the same position, allowing them to capture greater rents from reducing their marginal cost (shifting their position on the supply curve). we can sign Equation (3)’s cross-partial: \displaystyle\frac{\partial^2\pi}{\partial\Delta HR\partial D_m}\geq 0, which tells us that efficiency must increase (i.e., \Delta HR must increase and heat rate must decrease) when market-drought increases. However, this result and the assumption made to obtain it are only true for a plant that is not in drought. If a plant is in drought and market-drought D_m increases (more capacity/plants in the market are in drought), then increasing efficiency (or \Delta HR) would have a smaller positive effect on H since more of the supply curve remains relatively unchanged. In this case, \displaystyle\frac{\partial^2 H}{\partial\Delta HR \partial D_m}\leq 0, meaning that Equation (3) now has an ambiguous sign. Given this dichotomy in Equation (3)’s sign, we form the following hypotheses:

  • H1: Plants that are not in drought will improve their efficiency (decrease their heat rate) and experience an increase in capacity factor (due to marginal cost advantages from market-drought and/or their own efficiency) as market-drought increases.
  • H2: Plants that are in drought will improve their efficiency (decrease their heat rate) and experience a decrease in capacity factor as market-drought decreases.

We can explore the effect of own-drought on plants’ $\Delta HR$ choice by differentiating Equation (2) with respect to D_o, which yields

(4)   \begin{equation*}\frac{\partial^2\pi}{\partial\Delta HR \partial D_o}=(p-MC)q\frac{\partial^2 H}{\partial\Delta HR \partial D_o}-q\frac{\partial MC}{\partial D_o}\frac{\partial H}{\partial\Delta HR}-qH\frac{\partial^2 MC}{\partial\Delta HR \partial D_o}-q\frac{\partial H}{\partial D_o}\frac{\partial MC}{\partial\Delta HR}.\end{equation*}

Even with assumptions on the signs of the cross-partials in Equation (4), the equation still has an ambiguous sign. We attribute this ambiguity to our approach to modeling plants’ drought responses, particularly the dependence between plants’ own-drought reaction and market-drought summarized in Section 3.2’s three principal cases: how a plant’s profit-maximizing choice of efficiency (\deltaH R) depends on its own-drought D_o depends on market-drought D_m. Given this theoretical bulwark, we formulate the following hypothesis:

  • H3: Plants in drought have varying market-drought responses based on the severity of their own-drought condition.

4 Data

Our empirical tests of Section 3’s Hypotheses H0–H3 use monthly47Our analyses are performed at the monthly level because our plant-level data from the EIA are at the monthly level. Moreover, using daily or hourly data may not be appropriate since capacity factor changes or heat rate adjustments likely occur over longer periods of time than hours or days. mover-fuel-level data (hereafter referred to as PMFT for prime mover (PM) and fuel type (FT), respectively), where “mover” refers to prime mover (i.e., the generating technology, such as steam (ST) or combined-cycle (CC)) and fuel is either natural gas (NG) or coal (CO).48Other fuels, such as distillate fuel oil and petroleum, are present in the data, but most ST generating units use either natural gas or coal. All CC units use natural gas. All of our data are publicly available and span January 2010 through December 2020. Because only steam-powered generating units require cooling water, our final analysis is restricted to plants that use steam or combined-cycle generators. Moreover, for plants that use multiple steam-powered units with different coal types, we aggregate each unit’s data into one steam-powered coal-fired (ST-CO) observation. For example, if plant Z has a steam-powered bituminous coal-fired unit and a steam-powered refined coal-fired unit, our data combine both units’ data into one ST-CO entity observed over time. We apply a similar aggregation process to combined-cycle plants insofar as we combine the separate data on the gas and steam turbines into one CC-NG entity observed over time.

Our main electricity data sources are the EIA’s Form EIA-923 and Form EIA-860. We obtain PMFT-level generation in MWh, fuel consumption in MMBtu, prime mover type, and fuel type from Form EIA-923. We obtain plant location (i.e., city, county, zip, state, and coordinates), plant sector, plant balancing authority area, and generator-level nameplate capacity from Form EIA-860. Plant-level nameplate capacity is calculated by summing the nameplate capacity of all generators at a plant. For plants with multiple generators of the same PMFT combination, we also create PMFT-level nameplate capacity by summing the nameplate capacity of generators with the same PMFT combination. Total renewable generation in each balancing authority area is calculated using data from the EIA’s Form EIA-923 by summing the generation of all renewable plants within each area in each month. Finally, we obtain monthly Henry Hub natural gas prices from the EIA’s natural gas data page.

Our measure of plant-level generation is capacity factor, which is our first dependent variable.49The capacity factor ranges from zero to one, where zero denotes no electricity produced and one denotes full usage of a generating unit’s capacity.,50Since our analyses occur at the monthly level, we aggregate nameplate capacity to the month level by multiplying raw nameplate capacity by the number of hours in a given month. For example, if an ST-NG generating unit has a nameplate capacity of 100 MW and we consider the month of June, then we multiply 100 MW by 720 (the number of hours in June) to calculate that unit’s month-level capacity of 72,000 MWh. This choice allows us to account for differing plant sizes/capacities. We divide generation by monthly nameplate capacity in each month to construct PMFT-level capacity factor. Our measure of efficiency is plant-level heat rate, which is our second dependent variable. We divide fuel consumption by generation in each month to construct heat rate in MMBtu/MWh. In addition, we drop all observations with outlier (and potentially erroneous) values for heat rate, specifically dropping all observations with a heat rate greater than 100 MMBtu/MWh.51The California Energy Commission’s Energy Almanac website (https://ww2.energy.ca.gov/almanac/electricity_data/web_qfer/Heat_Rates_cms.php) lists heat rates as high as 82 MMBtu/MWh, while Linn, Mastrangelo, and Burtraw (2014) have a maximum average annual heat rate of 30 MMBtu/MWh for coal plants. Our relatively lax cutoff of 100 MMBtu/MWh attempts to balance these possible bounds of the heat rate spectrum while allowing for possibly realistic spikes in heat rate. Using a more restrictive cutoff of 30 MMBtu/MWh produces a mix of the same and differing results as we get from using the 100 MMBtu/MWh cutoff. We prefer our 100 MMBtu/MWh cutoff to allow for the full range of potentially extreme heat rate responses under extreme weather, which can impact fuel acquisition costs and load conditions.,52As of 2021, the average heat rate is 10 MMBtu/MWh for gas- and coal-fired steam generating units and 7.5 MMBtu/MWh for gas-fired combined-cycle generating units (US EIA, 2021).

We obtain data on our demand-side control variables from the US Federal Energy Regulatory Commission’s (FERC) Form 714. This source provides monthly load and net interchange in MWh at the balancing authority area level. Load is a measure of total monthly electricity demand in each month, allowing us to explicitly control for electricity demand. The net interchange variable is essentially a measure of net imports/exports. It enables us to control for transmission heterogeneity across balancing authority areas that may permit some areas to better respond to drought via greater electricity imports from other areas.

Our measure of drought is the PDSI. The PDSI uses precipitation and temperature data to estimate relative dryness using a physical water balance model, which enables it to account for climate change’s effects on drought (National Center for Atmospheric Research, 2022). The index ranges from –10 to 10, where values below –1 indicate drought conditions and decreases in the PDSI constitute decreases in water supply. We use a novel data set named gridMET from the Climatology Lab at the University of California Merced that provides daily PDSI measurements at a 4km or 1/24th degree grid cell resolution for the contiguous United States from 1979 to present.53To be specific, gridMET provides PDSI measurements at the centroids of each 4km or 1/24th degree grid cell spanning the contiguous United States.,54We aggregate gridMET’s daily PDSI measurements to the month level by taking the simple average of daily PDSI across all days in each month.

Figure 3. Snapshot of gridMET Data, February 2010

gridMET’s high spatial resolution enables us to construct a nearly plant-level measure of drought conditions using PDSI data from the grid cells closest to each plant.55Obtaining truly plant-level drought conditions would require measuring or observing water supply or PDSI at each plant’s water source or using a hydrological model to estimate drought conditions at each plant’s water source. The former is unavailable to us, and given the granularity of gridMET, the latter is left to future work. For each plant in our sample, we identify the 10 nearest 4km grid cell centroids to the plant and calculate the inverse-distance-weighted (IDW) average PDSI across the 10 PDSI values. That is, for plant p in month-year t with nearest grid cells g_i=1,\dots,10 each possessing raw PDSI values RP_{g_it}, we construct their IDW PDSI PDSI_{it} using

(5)   \begin{equation*}PDSI_{it}=\displaystyle\sum_{g_i=1}^{10}\omega_{g_{i}} RP_{g_it},\end{equation*}

with the normalized weights \omega_{g_i} calculated using \omega_{g_i}=\displaystyle\frac{u_{g_i}}{\sum_{g_i=1}^{10}u_{g_i}}, where u_{g_i}=\displaystyle\frac{1}{d(l_i,l_{g_i})} and d(l_i,l_{g_i}) is the geodetic distance between plant i and grid cell g_i‘s centroid.

Using EIA 860’s data on generator nameplate capacity and the gridMET PDSI data, we calculate each (market or nonmarket) area’s market-drought, defined as the proportion of capacity in drought in each month.56We also estimate our econometric models using county-level PDSI (obtained from the Centers for Disease Control and Prevention National Environmental Health Tracking Network’s website (https://data.cdc.gov/Environmental-Health-Toxicology/Palmer-Drought-Severity-Index-1895-2016/en5r-5ds4/data)) as the own-drought measure (still using gridMET PDSI for calculating market-drought); select county-level PDSI results are available in Appendix F. The results from using county-level PDSI for own-drought are different than our current gridMET PDSI measure for own-drought, varying from having more parameter estimates that are consistent with our theory to no significant estimates at all. These county-level PDSI results are less credible in our context due to their lower spatial resolution, which may confound plant-level effects. Moreover, the county-level PDSI data are only available until December 2016. The estimation results using county-level PDSI are available upon request.,57A previous version of this project that did not use drought bins or consider the role of market-drought attempted to use the HUC8-level Drought Severity and Coverage Index, whose data were obtained by querying the US Drought Monitor’s REST or API service (whose information can be found at https://droughtmonitor.unl.edu/DmData/DataDownload/WebServiceInfo.aspx). However, this measure incorporates drought bins by construction and thus is not fit for use in our models. This variable is calculated in each month as the amount of capacity in drought (calculated by summing the capacities of all plants in drought, that is, with PDSI_{it}\leq -1, in a given month) divided by the total capacity (calculated by summing the capacity of all plants in a given month). We construct this variable for both total capacity (i.e., across all PMFTs) and for the following key PMFTs: natural-gas-fired steam generation (ST-NG), natural-gas-fired combined-cycle generation (CC-NG), and coal-fired steam generation (ST-CO).

Figure 4. Mean Monthly PDSI by Market Area

Notes: Averaged over all plants in each area. Recall that PDSI≤ −1 constitutes being in drought.

Figure 5. Mean Monthly PDSI by Nonmarket Region

Notes: Averaged over all plants in each region. Recall that PDSI≤ −1 constitutes being in drought.

5 Econometric Framework

Our econometric analyses test our plant-level efficiency and capacity factor response hypotheses from Section 3 through several approaches. We begin by testing our market versus nonmarket area Hypothesis H0 using a binary own-drought indicator (Section 5.1). We then shed more light on H0 by using a categorical own-drought variable representing no-drought, mild drought, moderate drought, and severe drought conditions instead of a binary own-drought indicator (Section 5.1). Next, we test our market-drought Hypotheses H1 and H2 by estimating the effect of market-drought interacted with a binary own-drought indicator on market plants (Section 5.2.1).

Finally, we allow own-drought to vary in severity to test H3 by estimating the effect of market-drought interacted with a categorical own-drought variable representing no-drought, mild drought, moderate drought, and severe drought conditions (Section 5.2.2). We estimate each approach across all generation technologies that are susceptible to drought (i.e., all technologies that use a steam or combined-cycle prime mover, namely ST or CC prime mover plants) and also broken out by key PMFTs (prime mover PM and fuel type FT combinations) to allow responses to differ by technology (since operating cost and intrinsic efficiency differ across technologies).58Our key PMFTs are CC-NG (combined-cycle natural gas), ST-NG (steam natural gas), and ST-CO (steam coal).

We use two-way fixed effects regression models in all of our approaches. To clearly compare outcomes between drought and nondrought conditions, and to partially allow for nonlinear own-drought effects,59Eyer and Wichman (2018) also attempt to allow for nonlinear drought effects by interacting their continuous PDSI variable with categorical PDSI bins when studying drought’s effects on generation. we use a binary own-drought indicator and a categorical set of own-drought bins.60Market-drought is continuous and lies in [0, 1] but is calculated similarly to the binary own-drought indicator insofar as capacity whose own-drought P D S I_{i t} \leq-1 is counted as being capacity in drought. These binary and binned approaches also capture discrete changes that are potentially more salient to plants than finer-scale changes in water supply that would be captured by continuous PDSI. The PDSI bins are constructed in order of worsening severity as detailed in Table 3.61Our drought bin construction is based on the US Drought Monitor's drought classification table (which can be found at https://droughtmonitor.unl.edu/About/AbouttheData/DroughtClassification.aspx) and the National Weather Service Climate Prediction Center (https://www.cpc.ncep.noaa.gov/products/analysis_monitoring/cdus/palmer_drought/wpdanote.shtml).

We allow for heterogeneous responses by area by estimating all of our models separately for each US grid interconnection and RTO/ISO.62While all RTOs/ISOs run competitive wholesale electricity markets, they differ in size (geographic and capacity) and in what other types of electricity markets are in place (e.g., retail or capacity markets). For example, PJM has a retail electricity market, while NYISO does not. The major limitation of market-by-market analyses is a substantial loss in statistical power given our monthly data, which is why our interconnection-level analyses are preferred.,63To facilitate model computation and interpretation, we estimate separate models for each interconnection
and RTO/ISO instead of interacting a categorical interconnection or RTO/ISO variable with our own and
market-drought variables.
Moreover, in all of our specifications, we control for unobserved time-invariant plant-level characteristics (e.g., age, management style, and technology brand) through PMFT fixed effects. We control for unobserved entity-invariant factors that affect all plants in a region in the same manner and change over time (e.g., seasonal plant maintenance schedules, climatological fluctuations, government policies, and input costs)64Fuel costs can be affected by drought conditions when fossil fuel plants purchase more fuel in response to decreased hydropower generation under drought (Reuters, 2021; Jaffe, 2023) or in response to an increase in electricity demand stemming from drought’s accompanying ambient temperature increase. Both cases would cause fuel prices/costs to increase due to increased fuel demand. Because drought is also driving this aspect of marginal cost (fuel cost), our econometric models account for drought’s fuel cost effects with the PDSI measure and month-by-year-by-interconnect fixed effects. using month-by-year-by-interconnection fixed effects.

5.1 Own-Drought’s Effects on Market versus Nonmarket Plants

To test whether drought’s effects vary between market and nonmarket plants according to H0, we first use a binary drought indicator interacted with a binary market plant indicator. We omit the no-drought bin D_0 in our estimating equations to estimate drought’s effects on nonmarket and market plants relative to the no-drought case (i.e., no drought D_0 is our reference drought category). Our estimating equations then take the following forms:

(6)   \begin{equation*}CF_{ibrt}=\beta_0D_{1ibrt}+\beta_1\left(D_{1ibrt}\times MKT_i\right)+\boldsymbol{\theta}\mathbf{X}{ibrt}+\eta_i+\delta{rt}+\varepsilon_{ibrt},\end{equation*}

(7)   \begin{equation*}HR_{ibrt}=\alpha_0D_{1ibrt}+\alpha_1\left(D_{1ibrt}\times MKT_i\right)+\boldsymbol{\theta}\mathbf{X}{ibrt}+\eta_i+\delta{rt}+\varepsilon_{ibrt},\end{equation*}

where CF_{ibrt} is the capacity factor of plant PMFT i in balancing authority area b and interconnection r and month-year t, HR_{ibrt} is the heat rate of plant PMFT i in balancing authority area b and interconnection r and month-year t, and D_{1ibrt} is a dummy variable equal to one when a plant is in drought in month-year t and zero otherwise. MKT_i is an indicator variable equal to one if plant PMFT i is a market plant and zero otherwise, and \mathbf{X}{ibrt} is a matrix of control variables. \eta_i is a plant-PMFT-level fixed effect, \delta{rt} is a month-by-year-by-interconnect fixed effect, and \varepsilon_{ibrt} is an idiosyncratic error term. The control variables in \mathbf{X}_{ibrt} are load (i.e., electricity demand), net interchanges with other balancing authority areas, total solar generation, total hydroelectric generation, total wind generation, total nuclear generation, and total wind generation in area b and period t. Monthly Henry Hub natural gas prices are also included in our set of controls. We also control for PMFT-level capacity factor in heat rate models to account for the fact that heat rate can vary with usage or generation.65We also constructed a supply mix variable that measures the proportion of generation capacity from renewables in an attempt to further control for renewables’ impacts on plant drought responses. However, our combination of separate renewable energy controls and separate month and year fixed effects should allay any omitted variable bias concerns stemming from renewables.

Our parameters of interest for Equations (6) and (7) are {\beta_0,\beta_1} and {\alpha_0,\alpha_1}.66We use Stata’s nlcom command to calculate point estimates and standard errors for linear combinations of parameter estimates in all of our models. For consistency with our main panel data regression models (estimated using xtreg in Stata), we require nlcom to calculate t-statistics using the regression model’s residual degrees of freedom. \beta_0 and (\beta_0+\beta_1) measure drought's effect on capacity factor for nonmarket plants and market plants, respectively, while \alpha_0 and (\alpha_0+\alpha_1) measure drought's effect on heat rate for nonmarket plants and market plants, respectively. Following Section 3’s predictions and H0, we expect drought to decrease capacity factor for coal-fired market plants such that (\beta_0+\beta_1)<0 while increasing capacity factor for gas-fired market plants (as the market reallocates generation from water-intensive to less water-intensive plants) such that (\beta_0+\beta_1)>0. As for nonmarket plants' capacity factor, we expect drought to decrease capacity factor for all plant types such that \beta_0<0. Turning our attention to the heat rate effects parameters {\alpha_0,\alpha_1}, we expect drought to increase nonmarket plants' heat rate such that \alpha_0>0 and for market plants to decrease their heat rate in response to drought such that (\alpha_0+\alpha_1)<0.

Next, we allow own-drought’s effects to vary by drought severity by introducing the own-drought bins defined in Table 3:

(8)   \begin{equation*}CF_{ibrt}=\displaystyle\sum_{k=1}^3\tau_kD_{kibrt}+\displaystyle\sum_{k=1}^3\beta_k\left(D_{kibrt}\times MKT_i\right)+\boldsymbol{\theta}\mathbf{X}{ibrt}+\eta_i+\delta{rt}+\varepsilon_{ibrt},\end{equation*}

(9)   \begin{equation*}HR_{ibrt}=\displaystyle\sum_{k=1}^3\gamma_kD_{kibrt}+\displaystyle\sum_{k=1}^3\alpha_k\left(D_{kibrt}\times MKT_i\right)+\boldsymbol{\theta}\mathbf{X}{ibrt}+\eta_i+\delta{rt}+\varepsilon_{ibrt},\end{equation*}

where all variables except the D_{kibrt} terms are the same as in Equations (6) and (7). The D_{kibrt} terms are dummy variables equal to one when a plant's own-drought state is k\in K in month-year t and zero otherwise. Following the bin construction described in Table 3, D_{1ibrt} (k=1) denotes mild drought, D_{2ibrt} (k=2) denotes moderate drought, and D_{3ibrt} (k=3) denotes severe drought. The omitted drought bin is the no-drought bin D_{0ibrt} (k=0) so as to estimate the effects of varying drought severity relative to the no-drought case.

Our parameters of interest for Equations (8) and (9) here are {\tau_k,\beta_k} and {\gamma_k,\alpha_k}. These parameters allow us to speak to H3 applied to our market versus nonmarket plant analyses (i.e., that plants have varying drought responses based on the severity of their own-drought condition). The \tau_k terms and (\tau_k+\beta_k) measure drought severity k's effect on capacity factor for nonmarket and market plants, respectively, and the \gamma_k terms and (\gamma_k+\alpha_k) measure drought severity k's effect on heat rate for nonmarket and market plants, respectively. We again expect drought to decrease capacity factor for coal-fired market plants such that (\tau_k+\beta_k)<0 \forall k\in K while increasing capacity factor for gas-fired market plants such that (\tau_k+\beta_k)>0 \forall k\in K. We also again expect nonmarket plants' capacity factor to decrease in drought such that \tau_k<0 \forall k\in K.

Turning our attention to heat rate effects parameters {\gamma_k,\alpha_k}, we expect drought to increase nonmarket plants' heat rate such that \gamma_k>0 \forall k\in K, while market plants decrease their heat rate in response to drought such that (\gamma_k+\alpha_k)<0 \forall k\in K. A confirmation of H3 would be captured by differing estimates of \tau_k, (\tau_k+\beta_k), \gamma_k, and (\gamma_k+\alpha_k) at different drought severities k\in K. Moreover, worsened drought should intensify capacity factor effects and heat rate responses such that \gamma_1<\gamma_2<\gamma_3, \tau_1<\tau_2<\tau_3, (\gamma_1+\alpha_1)<(\gamma_2+\alpha_2)<(\gamma_3+\alpha_3), and (\tau_1+\beta_1)<(\tau_2+\beta_2)<(\tau_3+\beta_3).

In both the binary and binned own-drought models, we compare responses between market and nonmarket plants in five configurations: full sample, Eastern Interconnection, Western Interconnection, Texas versus Western Interconnection, and Texas versus Eastern Interconnection. In each configuration, we compare market plants to nonmarket plants. For example, the Eastern Interconnection setting compares responses by market plants in MISO, SPP, PJM, NYISO, and ISONE to responses by nonmarket plants in all of the nonmarket balancing authorities within the Eastern Interconnection (e.g., Florida Power & Light, Duke Energy). Because Texas operates its own grid interconnection apart from the Eastern and Western interconnections, we compare market plants in ERCOT to nonmarket plants in the Western and Eastern interconnections in separate configurations.

5.2 Own-Drought’s Market-Dependent Effects

5.2.1 Binary Own-Drought

To test whether own-drought’s market-dependent effects on market plant responses follow our competitive expectations in H1 and H2, we begin by using a binary drought indicator interacted with our continuous market-drought variable. We again omit the no-drought bin D_0 in our estimating equations to compare responses in drought to the no-drought case (i.e., no drought D_0 is our control or reference category). Our estimating equations then take the following forms:

(10)   \begin{equation*}CF_{ibrt}=\beta_0M_{brt}+\beta_1D_{1ibrt}+\beta_2\left(D_{1ibrt}\times M_{brt}\right)+\boldsymbol{\theta}\mathbf{X}{ibrt}+\eta_i+\delta{rt}+\varepsilon_{ibrt},\end{equation*}


(11)   \begin{equation*}HR_{ibrt}=\alpha_0M_{brt}+\alpha_1D_{1ibrt}+\alpha_2\left(D_{1ibrt}\times M_{brt}\right)+\boldsymbol{\theta}\mathbf{X}{ibrt}+\eta_i+\delta{rt}+\varepsilon_{ibrt},\end{equation*}

where M_{brt} is the proportion of balancing authority area b's thermoelectric capacity that is in drought in month-year t (market-drought) and all other variables are the same as in Equations (6)–(9).

Our parameters of interest here are {\beta_0,\beta_2} and {\alpha_0,\alpha_2}. More specifically, when considering plants' responses in drought, we are interested in (\beta_0+\beta_2) and (\alpha_0+\alpha_2), which capture market-drought's total marginal effect on capacity factor and heat rate, respectively, when a plant is in drought. \beta_0 and \alpha_0 alone measure market-drought's effect on capacity factor and heat rate, respectively, when a plant is not in drought. In the context of Section 3's predictions, we expect capacity factor to (1) increase with or be unaffected by increasing market-drought for plants not in drought and (2) decrease with decreasing market-drought for plants in drought; these are exactly Hypotheses H1 and H2, respectively.

For a plant in drought, their expectation follows from recognizing that decreasing market-drought is akin to approaching case 2 from case 1. Capacity factor for these plants should decrease with less of the market being in drought (lower market-drought) since that amounts to less of the supply curve being shifted along with the plant in drought, leaving them to bear greater losses in their probability of being inframarginal/marginal (thereby reducing their capacity factor). For a plant not in drought, an increase in market-drought means that more of the market is shifted up the supply curve, which increases the probability and frequency of a plant being inframarginal/marginal and manifests as an increase in the plant's capacity factor. All of this means that we expect

    \[\beta_0>0,\left(\beta_0+\beta_2\right)>0.\]

As for heat rate, we expect it to (1) decrease with or be unaffected by increases in market-drought for plants not in drought and (2) decrease with decreasing market-drought for plants in drought. These are once again Hypotheses H1 and H2, respectively. This means that we expect

    \[\alpha_0 \lesssim 0,\left(\alpha_0+\alpha_2\right)>0.\]

5.2.2 Binned Own-Drought

We next test Hypothesis H3 (whether own-drought's market-dependent effects vary with own-drought severity) by again introducing the full drought bin set K={0,1,2,3} into our market-drought estimating Equations (10) and (11):

(12)   \begin{equation*}CF_{ibrt}=\sum_{k=1}^3\tau_kD_{kibrt}+\beta_0M_{brt}+\sum_{k=1}^3\beta_k\left(D_{kibrt}\times M_{brt}\right)+\boldsymbol{\theta}\mathbf{X}{ibrt}+\eta_i+\delta{rt}+\varepsilon_{ibrt},\end{equation*}

(13)   \begin{equation*}HR_{ibrt}=\sum_{k=1}^3\gamma_kD_{kibrt}+\alpha_0M_{brt}+\sum_{k=1}^3\alpha_k\left(D_{kibrt}\times M_{brt}\right)+\boldsymbol{\theta}\mathbf{X}{ibrt}+\eta_i+\delta{rt}+\varepsilon_{ibrt},\end{equation*}

where all variables are the same as in Equations (8) and (9).

Our parameters of interest here are \beta_k and \alpha_k for k\in{0,1,2,3}. To be specific, when considering plants' responses in drought, we are interested in (\beta_0+\beta_k) and (\alpha_0+\alpha_k), which capture market-drought's total marginal effect on capacity factor and heat rate, respectively, when a plant is in drought bin k. \beta_0 and \alpha_0 alone measure market-drought's effect on capacity factor and heat rate, respectively, when a plant is not in drought. Our expectations about the signs of \beta_k and \alpha_k are the same as in Section 5.2, albeit extended to the full set of drought bins:

    \[\beta_0,\left(\beta_0+\beta_1\right),\left(\beta_0+\beta_2\right),\left(\beta_0+\beta_3\right)>0,\]

and

    \[\begin{gathered}\alpha_0 \lesssim 0 \\left(\alpha_0+\alpha_1\right),\left(\alpha_0+\alpha_2\right),\left(\alpha_0+\alpha_3\right)>0\end{gathered}\]

Hypothesis H3 is tested by verifying whether (\beta_0+\beta_1)\neq(\beta_0+\beta_2)\neq(\beta_0+\beta_3) and (\alpha_0+\alpha_1)\neq(\alpha_0+\alpha_2)\neq(\alpha_0+\alpha_3) (i.e., market-drought has different effects at different own-drought conditions).

6 Results

In this section, we report graphical representations of our econometric models’ parameter estimates and briefly contextualize them within our hypotheses. A complete discussion of our results’ implications within our institutional and theoretical framework is available in Section 7. We focus on results for specifications that display statistically significant effects, which were estimated with data from November 2014 onward to eliminate the influence of unusual load data before November 2014,67The culprit is MISO’s load data pre-November 2014, so for consistency across all of our specifications, we estimate the Western Interconnection and Texas models using only post-November 2014 data as well. and were estimated without units that had zero generation in one or more years68We interpret zero generation in one or more years as signifying that a plant is closing or is in the process of reconfiguring its generation method (e.g., switching from coal to natural gas generation). to reduce the noisiness of our sample. The regression tables referenced in this section can be found at the end of the paper. Several specifications generated significant results that contradict our theoretical hypotheses; a full discussion of the possible mechanisms behind these results is provided in Section 7.

Finally, every mention of “all technologies” or “drought-susceptible” units in this section refers to specifications estimated without distinguishing by any one key PMFT but rather on all units that are susceptible to drought (i.e., all ST and CC prime mover units). This is equivalent to allowing responses to be co-optimized across all ST and CC prime mover units regardless of the fuel they use. Following the setup in Section 5, all results stem from estimating our regression models separately for each interconnection to maximize our models’ statistical power.69Estimating our models separately for each RTO/ISO largely resulted in insignificant drought effects.

Recognizing that drought persistence or frequency likely matters for whether or not plants choose to respond along either margin (capacity factor or heat rate), we also present subanalyses of our specifications applied to subperiods of our full sample period in which drought was persistent or frequent in each market area. The subperiods for each interconnection were selected by using the National Integrated Drought Information System’s Historical Data and Conditions tool (which can be found at https://www.drought.gov/historicalinformation?dataset=0selectedDateUSDM=20111108) to visually identify subperiods between January 2010 and December 2020 in which each interconnection experienced frequent or persistent drought.70The subperiods for each interconnection are 2015–2017 for the Eastern Interconnection, 2018–2019 for the Western Interconnection, and 2018–2019 for Texas.,71Our drought-intensive years results omit the full sample to focus on interconnection-level periods of frequent or persistent drought rather than try to define such periods for the entire contiguous United States. We present results from these drought-intensive years subanalyses when they are statistically and economically significant.

6.1 Own-Drought’s Effects on Market versus Nonmarket Plants

For our binary own-drought models, the dots plotted in the "Nonmarket" portion of the graphs in this section are point estimates of the own-drought dummy D_1's coefficient \beta_0 for capacity factor results or \alpha_0 for heat rate results and represent drought's effects on nonmarket plants. The dots plotted in the "Market" portion of the graph are point estimates of the summed coefficients (\beta_0+\beta_1) for capacity factor results or (\alpha_0+\alpha_1) for heat rate results and represent drought's effect on market plants. The bars above and below each dot represent the point estimate's 95 percent confidence interval. For our binned own-drought models, we report our estimates in tables to avoid interpreting overly cluttered graphs.

6.1.1 Capacity Factor Results

Graphically, a confirmation of our market versus nonmarket plants capacity factor Hypothesis H0 using binary own-drought is denoted by a dot above the zero line in this section’s figures for natural-gas-fired market plants, below the zero line for coal-fired market plants, and below the zero line for all nonmarket plants regardless of fuel type. We generally find that gas-fired market plants respond as we expect, experiencing increased capacity factor when in drought as a result of the market reallocating generation to less water-intensive (and therefore lower cost despite drought’s effects) gas-fired plants. Figure 6 displays this expected result for CC-NG plants (which we focus on since ST-NG units tend to be peaker plants that do not produce as much electricity). However, we also find that nonmarket gas-fired plants experience the same capacity factor effect as their market plant counterparts, indicating that nonmarket operating utilities or entities are likely engaging in fleet-wide generation reoptimization during drought. Nonmarket gas-fired plants’ operators may also be engaging in sufficient bilateral trading in drought to mimic a market environment.

Figure 6. Binary Own-Drought’s Effects on Market versus Nonmarket Plants: CC-NG Capacity Factor

Notes: Standard errors are clustered at the plant-level.

As shown in Table 4’s binned own-drought results, allowing own-drought to vary in severity reveals that own-drought’s effects on gas-fired plants intensify with drought severity (i.e., more severe drought elicits larger capacity factor increases). For our full sample and Eastern Interconnection results, we find that market plants’ capacity factor increases are twice as large in severe drought D_3 than in mild drought D_1. Nonmarket plants again experience the same capacity factor increases as market plants, but they do not grow as much with worsening drought severity, possibly reflecting the limitations of fleet-wide generation reoptimization or extensive bilateral trading compared to wholesale markets’ centralized transactions.

As for coal-fired plants, we find largely null drought effects for both market and nonmarket plants.72The Western Interconnection is omitted from our coal models since it does not have sufficient coal generation for parameter estimation during our sample. However, focusing on drought-intensive years reveals the expected decreases in capacity factor for Texas market plants (Figure 7).

Figure 7. Binary Own-Drought’s Effects on Market versus Nonmarket Plants: ST-CO Capacity Factor, Drought-Intensive Years

Notes: Standard errors are clustered at the plant-level.

Moreover, as shown in Table 5, allowing own-drought to vary in severity reinforces the binary drought results for Texas coal-fired market plants displayed in Figure 7. As with gas-fired market plants, worsening drought severity also has the same effect of intensifying capacity factor effects: capacity factor decreases grow in magnitude with more severe drought, with effects nearly doubling from mild to moderate drought. However, drought’s effect disappears under severe drought. Because the drought-intensive period for Texas (2018–2019) comes after an extensive period of coal-fired plant retirements and wind power increases, this result may reflect the baseload of coal generation remaining online and unaffected despite cost increases.

6.1.2 Heat Rate Results

A graphical confirmation of our market versus nonmarket plants heat rate Hypothesis H0 using binary own-drought is denoted by a dot above the zero line for nonmarket plants and below the zero line for market plants regardless of fuel type. We only find significant heat rate responses in Western Interconnection market plants, as shown in Figures 8 and 9. Figure 8 (which restricts responses to be equal across all PMFTs) shows that Western Interconnection market plants (which are all located in CAISO) decrease their heat rate when in drought. Estimating our binary drought Equation (6) by key PMFT uncovers the fact that this overall effect is driven by ST-NG units, which reduce their heat rate substantially when in drought (Figure 9).

The average heat rate of CAISO ST-NG units in our final analysis sample is approximately 20.184, well above the CAISO average of 14.170 across all plant types and the average heat rate of CAISO CC-NG units (approximately 8.034). This is consistent with the fact that ST-NG units are mostly peaker plants that mainly serve peak demand periods and are required to quickly ramp up to a certain generation level, making them much less efficient and costlier to run than their combined-cycle (CC-NG) counterparts. When these costlier units are in drought, they face stronger incentives to minimize costs through efficiency improvements than other types of plants since they are called upon to generate infrequently. That is, their opportunities to be marginal or inframarginal are few and far between compared to baseload natural gas (CC-NG) plants, which serves to intensify competition among ST-NG peakers during drought. This intensified competition manifests in the form of sizable heat rate reductions (efficiency improvements) during drought.

Figure 8. Binary Own-Drought’s Effects on Market versus Nonmarket Plants: Heat Rate, All Technologies

Notes: Standard errors are clustered at the plant-level.

Figure 9. Binary Own-Drought’s Effects on Market versus Nonmarket Plants: ST-NG Heat Rate

Notes: Standard erros are clustered at the plant-level.

Similar to our capacity factor results, allowing own-drought to vary in severity reveals that Western Interconnection market plants intensify their heat rate decrease under more severe drought. Considering all generating technologies equally, Table 6 shows that the heat rate decrease in Western Interconnection market plants is larger in severe drought than in mild drought, but the difference is relatively small. Focusing on binned own-drought effects on ST-NG units in Table 7 shows that similar to binary own-drought’s heat rate effects, these peaker units are driving the overall binned own-drought effects. Western Interconnection market plants decrease their heat rate by about 23 percent more in severe drought than in mild drought.

6.2 Own-Drought’s Market-Dependent Effects on Market Plants

The interpretation of the graphs in this subsection is as follows. In our binary own-drought model results, the no-drought or "D0" portion shows market-drought's effect when a plant is not in drought, and the drought or "D1" portion shows market-drought's effect when a plant is in drought (regardless of drought severity). Thus, the plotted dots in the no-drought (D0) portion are point estimates of market-drought's marginal effect when a plant is not in drought \beta_0 for capacity factor or \alpha_0 for heat rate. Meanwhile, the plotted dots in the drought (D1) portion are point estimates of market-drought's total marginal effect when a plant is in drought (\beta_0+\beta_2) for capacity factor or (\alpha_0+\alpha_2) for heat rate.

Moreover, in our binned own-drought model results, the no-drought or D0 bin refers to market-drought's effect when a plant is not in drought, and the D1 bin refers to market-drought's effect when a plant is in mild drought. Bin "D2" refers to market-drought's effect when a plant is in moderate drought, and "D3" refers to market-drought's effect when a plant is in severe drought. The plotted dots are therefore the point estimates of each drought bin k's respective \beta_0 (market-drought's effect when a plant is not in drought) or (\beta_0+\beta_k) (market-drought's total marginal effect when a plant is in drought bin D_k) for capacity factor or \alpha_0 (market-drought's effect when a plant is not in drought) or (\alpha_0+\alpha_k) (market-drought's total marginal effect when a plant is in drought bin D_k) for heat rate. The bars above and below each dot in both the binary and binned own-drought model results represent the point estimate's 95 percent confidence interval.

6.2.1 Capacity Factor Results

A graphical confirmation of our market-drought capacity factor Hypotheses H1 and H2 is denoted by a dot above the zero line in both the no-drought and drought portions of the graphs. Beginning with our binary own-drought model results, we find that market plants in our full sample and Eastern Interconnection specifications experience exactly the expected capacity factor effects when not in drought and when in drought. Specifically, an increase in market-drought when a plant is not in drought increases their capacity factor as more plants in the market get shifted up the supply curve, while a decrease in market-drought when a plant is in drought decreases their capacity factor as less of the market gets shifted up the supply curve while the plant in drought still gets shifted up. Figures 10 and 11 show this for all technologies and CC-NG units, respectively.

Figure 10. Binary Own-Drought’s Market-Dependent Effects on Capacity Factor, All Technologies

Notes: Standard errors are clustered at the plant-level.

Figure 11. Binary Own-Drought’s Market-Dependent Effects on CC-NG Capacity Factor

Notes: Standard errors are clustered at the plant-level.

Allowing own-drought to vary in severity for our all technologies specification shows that worsening own-drought severity potentially intensifies market-drought’s effects (Figure 12) as it did own-drought’s effects in the prior subsection, albeit meagerly and limited to our full sample estimation.

Figure 12. Binned Own-Drought’s Market-Dependent Effects on Capacity Factor, All Technologies

Notes: Standard errors are clustered at the plant-level.

The lack of significant responses in the Western Interconnection and Texas is likely due to those regions having less market plants with which to identify market-drought responses counts.73The only market area in the Western Interconnection is CAISO, and the only market area in Texas is ERCOT. On the other hand, the Eastern Interconnection contains MISO, SPP, PJM, NYISO, and ISONE. However, we actually find that Texas ST-CO market plants experience our expected market-drought capacity factor effects during the state’s drought-intensive years of 2018–2019 (Figure 13). Allowing own-drought to vary in severity further reveals that this effect during drought-intensive years is again present when a plant is not in drought, and it is driven solely by mild own-drought when a plant is in drought (Figure 14). These findings may indicate that coal-fired plants in Texas are especially sensitive to persistent or frequent own-drought when it interacts with market-drought conditions.

Figure 13. Binary Own-Drought’s Market-Dependent Effects on ST-CO Capacity Factor, Drought-Intensive Years

Notes: Standard errors are clustered at the plant-level.

Figure 14. Binned Own-Drought’s Market-Dependent Effects on ST-CO Capacity Factor, Drought-Intensive Years

Notes: Standard errors are clustered at the plant-level.

6.2.2 Heat Rate Results

In this final subsection, a graphical confirmation of our market plant heat rate Hypotheses H1 and H2 is denoted by a dot below the zero line in the no-drought (D0) bin and a dot above the zero line in all drought bins (D1, D2, D3). We find little evidence of market plants adjusting their heat rate at all when not in drought, basically limited to CC-NG plants in Texas. We find essentially no evidence of market plants in drought decreasing their heat rate when market-drought decreases, except for ST-NG Eastern Interconnection plants in severe drought. Thus, market-drought does not appear to factor into market plants’ own-drought heat rate responses. Another factor at play for heat rate is plant planning horizons. Even with persistent or frequent drought, plants may lock in their operational expenses and strategies in blocks of months or annually, which is behavior that is masked by our monthly data and analyses.

7 Discussion

Our empirical analyses largely confirms our market versus nonmarket plant hypotheses for drought’s effects on capacity factor and heat rate. We find that natural-gas-fired market plants experience capacity factor increases when in drought, while coal-fired market plants experience capacity factor decreases when in drought, reflecting the allocative efficiency of wholesale electricity markets in shifting generation from water-intensive (coal) plants to less water-intensive plants (natural gas). Extending our analyses to include the role of market-drought reveals that only capacity factor effects are significantly affected by market-drought and consistent with our theoretical predictions; we find that nonmarket and market plants’ heat rates are mostly unresponsive to own-drought and market-drought. However, our results are greatly dependent on region and, to a lesser extent, drought frequency and persistence. This points to both statistical power issues in our sample as well as possible market failures in the Western Interconnection and Texas, where transmission issues (Buchele, 2023) combined with high levels of renewable generation (US EIA, 2023b) may be at fault.

We also find evidence of worse own-drought severity intensifying capacity factor effects. This makes sense as worsened drought conditions amount to larger cost shocks (i.e., severe drought imparts a larger efficiency loss and consequent marginal cost increase to plants than mild drought does) that should then elicit larger shifts within wholesale electricity supply curves. Our results overall highlight the importance of market structure due to the differing ways that costs are treated under different market structures.

Our results mostly extend prior research by assessing two previously unexplored channels: the role of market structure and the role of market-drought in plants’ drought responses. We can measure plant-level effects in both channels more precisely than prior work through our high-resolution PDSI data. Our work follows some previous research in studying drought’s generation effects (Mamkhezri and Torell, 2022; Qiu et al., 2023), but we use capacity factor rather than generation to account for differing plant sizes. Moreover, we follow research like Eyer and Wichman (2018) in studying large regions of the contiguous United States under the universe of drought events in our sample period rather than studying individual regions or single drought events (Scanlon et al., 2013; Mamkhezri and Torell, 2022). Finally, much of the research on the relationship between drought and thermoelectric power plants exists within the engineering literature (van Vliet et al., 2012; van Vliet, Vögele, and Rübbelke, 2013; van Vliet et al., 2016; Ganguli, Kumar, and Ganguly, 2017; Kern and Characklis, 2017). We extend the nascent and equally important research on this relationship from an economic perspective.

We also observe multiple instances of unexpected or counterintuitive results. The most notable is nonmarket plants experiencing the same capacity factor effects due to drought as market plants. The primary and most likely explanation for this is nonmarket plant operating utilities or entities engaging in fleet-wide generation reoptimization, that is, shifting their generation from water-intensive to less water-intensive plants when drought occurs by manually changing generation across their fleet. This behavior mimics the actions of a centralized wholesale electricity market, which accomplishes the same result but through a merit order based on each plant’s generation cost. Nonmarket utilities or entities may also augment their bilateral trading efforts with other nonmarket entities during drought in an effort to maintain reliability during extreme weather events.74For example, the North Carolina-based utility Duke Energy recently braced for peak demand periods during summer heat waves in 2023 with bilateral trades and imports (WRAL News, 2023).

The next unexpected result is the extensive absence of heat rate responses among both market and nonmarket plants. We only find significant heat rate decreases from Western Interconnection market plants, mostly from peaker ST-NG units that probably face considerably stronger incentives to remain cost-competitive than other generating units like combined-cycle natural gas or coal units. Given the prevalence of combined-cycle natural gas (CC-NG) units and the nontrivial (but waning) presence of coal (ST-CO) units in the Eastern Interconnection, we expected these units to adjust their heat rate during drought and for market-drought to significantly affect the heat rate responses of the market plants that employ CC-NG or ST-CO generation. We attribute the lack of heat rate responses to unknown power plant planning horizons. Plants’ planning horizons for responding to potentially long-lived climactic factors like drought may be longer than our analyses’ time scale of a month such that month-to-month changes may not pick up plant heat rate adjustments. Central to this planning horizon mechanism is the possibility that the benefits of not adjusting heat rate at all outweigh the benefits of adjusting heat rate in response to drought. Riding out drought may be preferable to repeatedly adjusting heat rate, particularly if heat rate adjustments are not permanent and require that costs be incurred even when drought is no longer occurring. Despite the lack of plant heat rate responses in both our market versus nonmarket and market-drought models, we still observe considerable capacity factor effects in both modeling frameworks, indicating that certain markets (particularly those in the Eastern Interconnection) are functioning properly by reordering supply curves in a cost-minimizing fashion during drought and in different market-drought conditions.

We also expected more robust results from Western Interconnection and Texas CC-NG and ST-CO plants given their frequent exposure to drought conditions compared to Eastern Interconnection plants (which experience less drought events and enjoy greater water access overall). As shown in the prior section, much of the heat rate results stem from peaker ST-NG units, although CC-NG capacity factor results tend to be more in line with our expectations. However, frequent exposure to drought may actually work against these regions in our estimation process. The plentiful null effects for our market versus nonmarket and market-drought models are likely due to poor spatial variation in drought in the Western Interconnection and Texas. Plotting the spatial distribution of PDSI (as in Figure 3) over all months in our sample reveals that areas like CAISO tend to always almost completely be in drought or not in drought, supporting the poor spatial variation channel. Furthermore, as pointed out by an anonymous reviewer, overwhelmingly large drought impacts may mask heat rate adjustments; drought may increase certain plants’ heat rate so much that no plant-level adjustments can offset it. Finally, all of our results are tempered by our empirical methodology’s chief limitation: limited modeling of drought’s possibly nonlinear effects on plant operations.

In addition to increasing the amount of renewable energy on the grid, policy-based efforts to decarbonize the energy sector also include changes to the thermoelectric fleet such as plant retirements (mainly for coal-fired plants), retrofits (e.g., modifying coal plants to run on natural gas), and stricter emissions standards. These changes are especially important to consider in the context of drought as reliability concerns mount with the increasing frequency of extreme weather events in general. Policymakers are increasingly concerned with the fossil-fuel fleet’s ability to withstand extreme heat and cold events since this ability can impact the wholesale price of electricity and consequently affect retail electricity prices.75This has been the case with the Texas cold snap of February 2021 (DiSavino and Kelly, 2021). Our results show that thermoelectric plants’ drought responses are dependent upon fuel type (by way of water intensiveness) and region. That is, some areas’ markets appear to be functioning as intended when it comes to plant cost minimization in the face of extreme weather, but this result is specific to certain fuels and generating technologies. For example, we find that coal-fired plants tend to display significant effects only in drought-intensive years. This points to a need for policy to not only be area specific but also technology specific and weather dependent.

The importance of the dichotomy between competitive and noncompetitive market structures for electricity that we uncover is also relevant for policies aiming to incentivize extreme weather responses for power plants. A blanket policy for all natural-gas-fired power plants regardless of the type of market that they operate in, for example, would potentially limit the policy’s efficacy by allowing advantageous strategic compliance or efficiency losses due to differing market mechanisms. This is especially pertinent for nonmarket regions whose operating entities appear to mimic market areas in our results, since such regions may be well suited for market-based policies despite not formally operating a competitive wholesale market.76A good example of nonmarket entities formalizing their market-based tendencies is the Southeast Energy Exchange Market (https://southeastenergymarket.com/), which began operations in November 2022. Moreover, the apparent irrelevance of market-drought for plant-level heat rate adjustments that we find underscores the fact that own-drought is the only salient factor for plant-level decisions. That is, while our market-drought capacity factor results enhance our market versus nonmarket analyses by showing that markets are working as intended even in the face of market-level cost shocks, plants do not appear to account for such market-level drought impacts when making plant-specific decisions (capacity factor is largely a function of market forces and the merit order, not plant-level decisions). Thus, policies could benefit from focusing on regulating market-level operations rather than on plant-level regulatory approaches. Improving and expanding market mechanisms for wholesale power may ultimately spur greater grid resilience and efficiency than relying on plant-specific adjustments.77The recent expansion of CAISO’s Western Energy Imbalance Market and the development of SPP’s Markets+ are notable examples.

8 Conclusion

The transition to a decarbonized energy sector is a major part of society’s efforts to adapt to and mitigate climate change. This transition will take time to occur as renewable generating technologies are implemented, and therefore the behavior of existing fossil fuel plants takes center stage as extreme weather events (like drought) increase in frequency. Thus, it is important to understand how these plants respond to drought, whether electricity markets affect their responses in an efficient cost-minimizing manner, and how the extent of drought affects such responses. Prior work has studied generation responses without considering market structure, but we contribute additional perspectives by studying efficiency responses, responses in different market types (competitive markets versus nonmarket monopolistic utilities), and explicitly modeling the dependence of plant drought responses on market-drought conditions.

We use panel data on thermoelectric power plants’ operations and a novel high-resolution PDSI data set along with fixed effects regression models to examine whether wholesale electricity markets enact the expected capacity factor (generation reallocation) and efficiency (heat rate improvement by market plants) effects and how generating units respond to their own-drought condition under different market-drought conditions. The essence of our drought response framework lies in the fact that drought ultimately decreases plant efficiency and increases marginal cost in the absence of any adjustment by the plant. Our theoretical exposition on market plants versus nonmarket plants posits that market areas should engage in generation reallocation from water-intensive (coal) plants to less water-intensive (natural gas) plants and incentivize market plants to improve their efficiency (reduce their heat rate) during drought. In addition, nonmarket plants are not expected to experience either outcome.

Next, focusing on market plants, our theoretical market-drought exposition predict that plants’ drought responses along two margins (capacity factor and heat rate) depend on the extent of market-drought in their area. Plants in drought are expected to experience capacity factor decreases only if market-drought is relatively low. This is because lower market-drought corresponds to less of the market supply curve being shifted, leaving the plant that is in drought with greater losses in their probability of being inframarginal or marginal (i.e., of generating). Plants not in drought are expected to experience capacity factor increases only if market-drought is relatively high. This is because higher market-drought means that more of the plants in the market are shifted up the supply curve, which increases the probability of a plant not in drought being inframarginal or marginal. As for heat rate, plants in drought are expected to not lower their heat rate in response to drought if market-drought is high. This is because more of the supply curve is shifted up with the plant in drought when market-drought is high, eroding the incentives for such a plant to reduce its heat rate.

Through our econometric analyses, we generally find that market plants experience the capacity factor effects and, to a lesser extent, exhibit the heat rate improvements that we expect market areas to incentivize. However, these results depend on region, with capacity factor effects largely only appearing in the Eastern Interconnection and heat rate responses only appearing in the Western Interconnection. Our results also highlight peaker ST-NG plants as being especially sensitive to drought with respect to heat rate or efficiency adjustments. Our market-drought effects are quite muted for capacity factor (with minute effects again limited to Eastern Interconnection plants) and almost nonexistent for heat rate, indicating that only own-drought conditions matter for plant-level efficiency adjustments during drought. Moreover, many of our binned own-drought results display evidence of worsening drought severity intensifying capacity factor effects. Finally, drought persistence and frequency only factor into plant responses in a few market-technology scenarios, as evidenced by our limited significant results from focusing on drought-intensive years.

This paper’s theoretical framework and empirical results accentuate the need for area-specific and technology-specific policy within the water-energy nexus, particularly as it pertains to wholesale and retail costs within the greater scope of reliability. Effective electric reliability or cost-effectiveness policy likely cannot take any sort of blanket approach if efficiency and cost minimization are to be central tenets. As recent efforts to modernize and retrofit fossil fuel plants amid mounting reliability concerns have shown, policymakers are increasingly concerned with such plants’ ability to endure extreme weather events for the sake of providing power and ideally providing it at least cost. Competitive electricity markets are supposed to accomplish just that. We find that some areas’ markets are functioning as intended and incentivizing the right plants to generate more or less and improve their efficiency under drought. Interestingly, nonmarket plants are experiencing the same capacity factor effects as their market counterparts, which, combined with the results for market plants, emphasizes the dichotomy between competitive and noncompetitive market structures for electric policy; even nonmarket entities may be open to engaging in electricity markets.

Finally, the fact that market-drought matters for plant capacity factor points to the potential for expanded grid transmission to help with extreme weather resilience. Ongoing transmission expansion efforts can benefit from this research’s insights, particularly since we lack robust results in the Western Interconnection and Texas (which are both ridden with transmission issues). Transmission expansion can further the growth of wholesale electricity markets or even just market-reminiscent structures like the nascent Southeastern Energy Exchange Market, enabling increased access to the generation reallocation that we find in this paper.

Although our analyses use drought data at a high spatial resolution that allows us to construct IDW plant-level drought conditions, we still may not be capturing drought’s effects as accurately as possible. This is because a plant’s true drought conditions may only depend on the water supply in their cooling water source. Future research should explore the incorporation of hydrological models to better characterize true drought conditions at individual plants. In addition, our attempt at modeling nonlinear drought effects through drought bins may not be ideal. Future research should attempt to explicitly model such nonlinear effects.

Regression Tables


Appendix A: Drought’s Effects on Power Plant Efficiency and Marginal Cost

Thermoelectric power plants generate electricity by combusting a fossil fuel (e.g., coal or natural gas) and using the resulting heat to create steam that is then passed through a turbine to turn its blades and the rotor shaft of a generator, which then generates electricity. After passing through the turbine, the steam must then be cooled back into liquid form to be reused in the second step of the aforementioned process. Outside water must be withdrawn from a surface water source (or cooling tower in recirculating cooling systems78Recirculating cooling systems also withdraw water from surface water sources but at a much lower frequency that once-through cooling systems. As previously mentioned in the main text, the cost of this reduced water withdrawal frequency is higher water consumption, mostly through evaporation.) to be used as cooling water in plants’ cooling systems and the steam cooling process.

Figure 15 illustrates the generation and water usage processes for a plant with a recirculating cooling system (as evidenced by the presence of a cooling tower).79Graphically, the processes would be the same for a plant with a once-through cooling system: simply remove the cooling tower from the picture. A crucial component of a thermoelectric power plant’s cooling system is its condenser, which serves as a heat rejection mechanism for cooling/condensing used steam back into liquid form for reuse in the electricity generation process (Zubovic, 2021). Not only do condensers cool steam back into liquid form, but they also create a pressure sink that helps pull steam through the turbine. This affects the generation capacity of the turbine/generator (Zubovic, 2021) and consequently impacts the efficiency of the electricity generation process, which we elaborate on below.

Figure A1. Illustration of How Generation andWater Usage Occurs at Thermoelectric Power Plants

Notes: Figure source is US Geological Survey Water Science School (2018).

From an engineering perspective, drought’s water quantity and quality (temperature) effects chiefly affect the condenser’s operating conditions. The most important condenser condition parameter is condenser pressure, which is increased by both higher intake water temperatures (quality effect) and lower streamflow (quantity effect) (Putman and Harpster, 2000; Pattanayak, Padhi, and Kodamasingh, 2019). An increase in condenser pressure amounts to an increase in the endpoint pressure on the exhaust side of the turbine (since the cooling system is the first place that exhaust steam travels to after passing through the turbine, hence the endpoint term; the condenser is the endpoint for the plant’s water cycle). Continuing with the pressure sink terminology, this means that an increase in condenser pressure shrinks the sink, reducing its ability to pull steam through the turbine.80In engineering parlance, this increase in endpoint pressure is an increase in endpoint enthalpy. Absent an adjustment by the turbine, this rise in endpoint (or condenser) pressure reduces the generating capacity of the turbine as well as the generation level (i.e., less energy can be extracted from the same steam since it is moving through the turbine more slowly due to the sink shrinkage).

In practice, turbines do adjust to this rise in endpoint pressure: the turbine governor, which regulates the turbine’s rotational speed (Petrotech, 2017), increases the throttle to increase the steam flow (Lakovic et al., 2010; Pattanayak, Padhi, and Kodamasingh, 2019) and maintain the generation level. To achieve this increased steam flow, the fuel firing rate is increased (Lakovic et al., 2010), meaning that more fuel is combusted to generate the same amount of electricity. Recalling that heat rate (our measure of efficiency) is equal to the amount of fuel combusted divided by the amount of electricity generated, this result means that the heat rate has increased and efficiency has decreased due to the increase in condenser pressure. Other research that confirms this negative relationship between condenser pressure and efficiency includes Bhoi, Meta, and Bhojak (2015) and Hamanaka, Zhao, and Sharpe (2009).

Colman (2013) provides another avenue through which plant efficiency is affected by drought’s quality (temperature) effect by connecting increased intake water temperature with a heat engine’s Carnot efficiency. Carnot efficiency is the maximum possible efficiency achievable by a heat engine operating between two temperatures (Pisupati, 2020): a heat source temperature T_H (i.e., steam temperature) and a heat sink temperature T_C (i.e., cooling water temperature). Letting Q_H be the heat input (i.e., fuel combusted), Q_C be waste heat dissipated, and W be work done (i.e., MWh of electricity generated), let thermal efficiency be

    \[\eta_{t h}=\frac{W}{Q_H}\]

By the first law of thermodynamics, and the fact that energy cannot be completely converted to work W, the heat input (fuel combusted) Q_H must equal work done plus waste heat dissipated, meaning that

    \[\begin{gathered}Q_H=W+Q_C, \W=Q_H-Q_C .\end{gathered}\]

Thus, thermal efficiency can be rewritten as

    \[\eta_{t h}=\frac{Q_H-Q_C}{Q_H}.\]

Simplifying the equation for thermal efficiency and letting T_C = Q_C, T_H = Q_H be the temperatures of the heat sink (condenser) and heat source (steam), respectively, we obtain the equation for Carnot efficiency \eta_C:

    \[\eta_C=1-\frac{T_C}{T_H}.\]

Thus, for an increase in heat sink (condenser) temperature T_C (from an increase in intake water temperature due to drought), the maximum possible or Carnot efficiency decreases.

Appendix B

Figure B1. Map of US Balancing Authorities

Notes: Figure source is US EIA (2016).

Appendix C

Figure C1. Map of Balancing Authority Areas in the Western Interconnection

Notes: Figure source is Western Electricity Coordinating Council (2017).

Appendix D

Figure D1. Example of Electricity Dispatch Curve with Perfectly Inelastic Demand Curves

Notes: Figure source is US EIA (2012).

Appendix E

Once-through systems withdraw water, use it in the cooling process, and discharge it (at a warmer temperature) back to its source. Such systems are widespread across the eastern United States and were popular due to their low cost and simplicity (Union of Concerned Scientists, 2013). Recirculating systems withdraw water but at much lower volumes and rates than once-through systems because they use cooling towers or ponds to reuse withdrawn cooling water. These towers or ponds expose used cooling water to ambient air to cool it; some cooling water naturally evaporates as a result, and the remaining cooling water is reused in the steam cooling process (Union of Concerned Scientists, 2013). Consequently, recirculating systems have much higher water consumption volumes and rates than once-through systems (US EIA, 2014). Dry cooling systems use ambient air to cool steam, and can be categorized into two types: direct systems that use no water at all and indirect systems that use minimal cooling water kept in a closed system. Finally, hybrid cooling systems are a blend of dry and wet cooling.

Appendix F: Select Results Using County-Level PDSI for Own-Drought (gridMET PDSI for Market-Drought)

Figure F1. County-Level Binary Own-Drought’s Effects on Market versus Nonmarket Plants: CC-NG Capacity Factor

Notes: Standard errors are clustered at the plant-level.

Figure F2. County-Level Binary Own-Drought’s Market-Dependent Effects on CC-NG Capacity Factor

Notes: Standard errors are clustered at the plant-level.

Figure F3. County-Level Binary Own-Drought’s Market-Dependent Effects on Capacity Factor, All Technologies

Notes: Standard errors are clustered at the plant-level.

Figure F4. County-Level Binary Own-Drought’s Effects on Market versus Nonmarket Plants: Heat Rate, All Technologies

Notes: Standard errors are clustered at the plant-level.

Figure F5. County-Level Binary Own-Drought’s Market-Dependent Effects on CC-NG Heat Rate

Notes: Standard errors are clustered at the plant-level.

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CGO scholars and fellows frequently comment on a variety of topics for the popular press. The views expressed therein are those of the authors and do not necessarily reflect the views of the Center for Growth and Opportunity or the views of Utah State University.