Foundations9 min read

How Weather Drives U.S. Power Markets

A practical overview of how temperature, wind, solar, and storm patterns translate into electricity demand, generation output, and wholesale prices across the nine major U.S. ISO regions.

By the Weather Workbench Editorial TeamPublished Updated

Electricity is one of the only commodities that has to be produced and consumed at the same instant. There is no warehouse for power and no equivalent of an oil tanker waiting offshore. The grid is a real-time balancing act between supply and demand, and the variable that moves both sides of that balance harder than anything else is the weather. A heat wave in Texas, a snowstorm in New England, or a calm overnight period in the wind-rich Great Plains all reshape the short-term operating picture of the U.S. power system.

This article walks through the main weather-to-power transmission channels and explains why a single forecast revision can move billions of dollars in market positions across the day-ahead and real-time energy markets. It is written for analysts, traders, planners, and anyone trying to understand why their neighborhood utility is suddenly asking customers to conserve electricity at 6 p.m. on a Tuesday in August.

Demand: temperature is the dominant driver

The single most important weather variable for electricity demand is temperature. Across most of the United States, electricity load follows a U-shaped curve relative to outdoor temperature. The bottom of the U sits in the 60s — temperatures cool enough that buildings do not need air conditioning but mild enough that little heat is required. As temperatures rise above the high 60s, air conditioning load climbs steeply, with each additional degree adding hundreds of megawatts to a regional system. As temperatures fall below the low 60s, electric heating, heat pumps, and supporting equipment add load on the cold side of the curve.

The exact shape of the curve depends on the regional building stock. The Southeast, Texas, and California are heavily air-conditioned and weakly heated electrically, so summer dominates. The Pacific Northwest historically had cool summers and electric resistance heating throughout, so winter has been the system peak. New England and New York have traditionally been summer-peaking systems with heating-oil and gas furnaces, but that is shifting as buildings electrify under state climate laws.

Industry analysts use heating degree days (HDD) and cooling degree days (CDD), computed from daily mean temperature against a 65°F base, to convert raw temperature into a load-relevant index. A day with mean temperature of 90°F contributes 25 CDD; a day with mean temperature of 20°F contributes 45 HDD. Forecast departures from normal in HDD or CDD are the most-watched short-term load drivers across the natural gas and power desks.

Supply: wind, solar, hydro, and thermal availability

On the supply side, weather affects four major resource types. Wind output depends on hub-height wind speeds across hundreds of square miles of wind farms, and a single front passing through Oklahoma, Iowa, or West Texas can move thousands of megawatts within a few hours. Solar output depends on cloud cover and aerosol load (smoke from wildfires has periodically derated solar output across the entire West for days at a time). Hydroelectric capacity is set seasonally by snowpack and by precipitation runoff into the Columbia, Sacramento, and Missouri river systems. Thermal generation — coal, natural gas, nuclear — has weather sensitivity too: cooling water temperatures can derate plants in summer, and natural gas wellhead production can freeze off in extreme cold.

Each of these resource types has a distinct weather-to-output transfer function, and ISO operators must forecast each of them separately to build a credible day-ahead dispatch. Errors compound: a low-confidence wind forecast paired with a low-confidence load forecast can swing the system from comfortable reserves to emergency conditions within an operating hour.

Storms: the asymmetric tail risk

Beyond the steady-state weather drivers, severe storms create the asymmetric tail risk that defines the modern grid. Hurricanes and tropical systems can knock out distribution and transmission infrastructure across multi-state regions for days or weeks, with major historical examples including Sandy, Maria, Harvey, Helene, and Ian. Tornadoes and derechos sweep through SPP, MISO, and the southern PJM footprint each spring, taking transmission lines down faster than utilities can repair them. Ice storms across the Tennessee Valley, the Carolinas, and the Mid-Atlantic Piedmont produce some of the longest restoration timelines because the damage is distributed across thousands of distribution feeders.

These events are infrequent at any given location but practically certain to occur somewhere across the U.S. footprint each year. The reliability investments utilities make — undergrounding distribution, hardening transmission corridors, building mutual-aid networks — are largely shaped by the historical storm catalog.

Why a forecast revision moves prices

When the National Weather Service or major numerical weather model issues a revised forecast, the wholesale energy markets respond almost immediately. Day-ahead prices for the affected region adjust to reflect the revised load forecast and the revised wind and solar capacity factors. Real-time prices in the relevant ancillary services markets adjust to reflect the changing reserve requirements. Natural gas markets respond in parallel because gas-fired generation is the marginal resource in most regions and most hours.

The largest forecast-driven price moves come during periods of constrained supply. A heat dome forecast for ERCOT in late July can push day-ahead settled prices into the hundreds of dollars per megawatt-hour and trigger scarcity pricing additions on top of energy prices. A bomb cyclone forecast for ISO-NE in January can push New England gas basis prices to multiples of Henry Hub. These dislocations are when weather forecasting and energy trading intersect most consequentially.

What to watch on Weather Workbench

Weather Workbench surfaces the inputs that matter most to the U.S. power markets in one place: NWS gridpoint forecasts at city scale, climate-normal-based degree day departures, NWS active alerts, the Climate Prediction Center 6–10 and 8–14 day extended outlooks, GFS and European model anomaly comparisons, and U.S. Drought Monitor conditions. None of these are proprietary — they all come from federal agencies and public data sources — but pulling them into a single ISO-organized view is what makes the operational picture click. From there, professional traders, planners, and operators dig into their own paid data subscriptions for the specific contract or asset they are trading.

The next set of articles in this Learn section walks through individual data products in more depth, including how to read CPC outlooks, what HDD and CDD really measure, and how recent winter storms reshaped grid operations across the country.

Sources

Historical events and figures referenced in this article are drawn from the public-use federal and ISO sources listed below. No source is paywalled or proprietary.

  • National Hurricane Center Tropical Cyclone Reports (nhc.noaa.gov) — Hurricanes Sandy, Maria, Harvey, Helene, and Ian.
  • NWS Weather Prediction Center storm-event summaries — August 2020 Iowa derecho.
  • ISO market monitor reports (ERCOT settlement data; PJM, ISO-NE, and CAISO market monitor publications) — pricing dynamics during heat and cold events.
  • U.S. Energy Information Administration electric system data (eia.gov) — generation mix and demand context.