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06 Numbers and Powers

Forecast Europe’s Electricity Demand via Weather

Card No. 06·8008 · Updated · Standard formula, shown below

This guide explains how to use weather forecasts to anticipate electricity demand across Europe. You’ll learn to translate temperature, wind, and solar data into demand patterns, which helps with energy trading, grid management, and cost planning. No special software is needed—just access to weather data and a basic spreadsheet.

What You’ll Need

  • Access to a weather forecast service (e.g., national meteorological office, OpenWeatherMap, or ECMWF data).
  • A spreadsheet application (Excel, Google Sheets, or similar).
  • Historical electricity demand data for your region (optional but helpful for calibration).
  • Basic knowledge of how to use formulas in a spreadsheet.

Step-by-Step

  1. Identify your region and forecast horizon. Determine which European country or bidding zone you’re analyzing (e.g., Germany, France, Nord Pool). Decide if you need a day-ahead forecast (24-48 hours) or a shorter-term outlook. Weather forecasts are most reliable for the next 1-3 days.
  2. Collect the key weather variables. For each day, gather:
    • Average temperature (°C) – the single biggest driver of heating and cooling demand.
    • Wind speed at turbine hub height (typically 100m) – affects wind power output, which reduces net demand.
    • Solar irradiance (W/m²) or cloud cover – affects solar PV output.
    • Precipitation (mm) – can affect heating patterns and hydro generation.
  3. Estimate the temperature–demand relationship. For most of Europe, electricity demand rises when temperatures fall (heating) and also rises when temperatures are very high (cooling). A common approach is to calculate a “heating degree day” (HDD) and “cooling degree day” (CDD):

    HDD = max(0, 18°C – average temperature)

    CDD = max(0, average temperature – 22°C)

    Then, using historical data, find the linear relationship: Demand = base + a × HDD + b × CDD. If you don’t have historical data, a rough rule is that each HDD increases demand by about 0.3-0.5% of the baseline.
  4. Adjust for wind and solar output. High wind speeds reduce the need for conventional generation because wind turbines produce more. Similarly, sunny days reduce demand for gas or coal. Use a capacity factor for your region: e.g., onshore wind might have a capacity factor of 20-30%, offshore 35-45%. So, if installed wind capacity is 50 GW and the forecast wind speed gives a capacity factor of 0.3, then wind output = 50 × 0.3 = 15 GW. Subtract this from the gross demand.
  5. Account for seasonal and weekly patterns. Demand is generally lower on weekends and holidays, and higher on weekdays. In summer, demand peaks in the afternoon due to air conditioning; in winter, peaks are in the morning and evening. Apply a multiplier: e.g., weekend demand might be 90% of a typical weekday.
  6. Combine the effects into a forecast model. In your spreadsheet, create columns for each variable and a formula like:

    Forecast Demand = (Base + a×HDD + b×CDD) × (1 – wind_share) × (1 – solar_share) × day_type_factor

    Where wind_share = expected wind output / total generation capacity, and solar_share similarly.
  7. Validate and refine. Compare your forecast with actual demand data from the previous day. Adjust the coefficients (a, b, wind_share) to minimize errors. Over time, you’ll develop a model that works for your specific region.
  8. Use the forecast for decision-making. For trading, anticipate price spikes when demand is high and renewable output is low. For grid management, prepare for peak hours. For consumers, shift usage to off-peak times if prices are dynamic.

Common Mistakes

  • Using surface temperature instead of the temperature that affects heating. The 18°C base is a standard, but actual heating thresholds vary by building insulation. Calibrate with your data.
  • Ignoring wind and solar effects. In 2023, wind and solar supplied about 27% of EU electricity. Neglecting them can lead to large errors, especially on windy days.
  • Forgetting about daylight saving time and holidays. Demand patterns shift by an hour in spring/autumn, and public holidays can reduce demand by 5-10%.
  • Using a single temperature for a large country. Europe spans multiple climates; a weighted average of major cities is better.
  • Not updating your model. Energy efficiency and electrification (heat pumps, EVs) change the demand response over time.

Tips

  • Use the ECMWF’s ensemble forecasts for probabilistic predictions—they give a range of possible outcomes, not just one.
  • For day-ahead, the most accurate weather data is usually available from national meteorological services (e.g., DWD in Germany, Météo-France).
  • If you’re new, start with a simple linear model using only temperature, then add wind and solar later.
  • Track your forecast errors daily. A mean absolute error (MAE) of less than 3% of peak demand is considered good for a simple model.
  • Consider using a “degree-day” approach for heating: each degree below 18°C increases demand by roughly 0.4% of the winter baseline.

Troubleshooting

  • Forecast is consistently too high or too low. Check your base demand value. It may be outdated. Recalculate the base using the last 30 days of data.
  • Errors spike on windy days. Your wind capacity factor might be too high or too low. Look up the actual wind output (ENTSO-E publishes it) and adjust.
  • No historical data available. Use a simplified model: start with a baseline of 50 GW for a large country, then add 0.3 GW per HDD and subtract 0.2 GW per GW of wind output. You’ll need to refine later.
  • Weather forecast changes after you run the model. Run the model multiple times a day, especially if the forecast is volatile. Use the latest forecast for the closest hours.
  • Demand spikes that aren’t explained by weather. Check for major events (e.g., World Cup finals, extreme TV events) that cause simultaneous viewing and increased demand.

Frequently Asked Questions

Why does temperature affect electricity demand so much?

In Europe, heating is often electric (heat pumps, resistive heaters) or uses electricity for circulation pumps. When it’s cold, more heating is needed. Cooling is less common but growing, especially in southern Europe.

How accurate can this method be?

With a well-calibrated model, you can achieve a mean absolute error of 2-5% of peak demand for the next day. For longer horizons, errors grow due to weather uncertainty.

Do I need to use wind and solar data?

Yes, especially in countries with high renewable penetration like Germany or Spain. Wind and solar can reduce net demand by 20-30% on good days.

What is the best source for weather data?

For free, Open-Meteo or the GFS model via NOAA. For professional use, ECMWF or national services. Always use the same source consistently to avoid biases.

Can I use this method for a single city?

Yes, but you’ll need to adjust the coefficients. A city’s demand is smaller and more sensitive to local weather, so the model may be less stable.

How do I handle extreme weather events?

Extreme cold or heat can cause demand to spike non-linearly. Add a “stress” multiplier (e.g., 1.2 for temperatures below -10°C) to capture this.

Related

Method: the standard formula for this calculation, rounded as each result states. See how the calculators work or report an error.

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