El Niño Atlas

Methods

Every number on this site comes from official data, processed by published, repeatable rules. Sentences such as "Odds favour a drier-than-normal December–February" are assembled from the numbers by fixed rules, not written freely by a person or a machine.

El Niño status

Seasonal outlook

  1. We download the Copernicus Climate Change Service (C3S) seasonal forecast from ECMWF's SEAS5 model (system 51): every ensemble member, monthly means of 2 m temperature and total precipitation.
  2. We also download the same model's re-forecasts (hindcasts) for 1993–2016, for the same start month.
  3. Both are averaged over each 3-month season (for a forecast issued in November: December–February and February–April) and over each country, weighting each grid cell by how much of it lies inside the country and by its area.
  4. "Normal" is the middle third of all hindcast values for that country and season. The share of forecast members below, inside and above that range gives the odds of drier/normal/wetter (or cooler/normal/warmer).
  5. Headline rules: "likely" when one side has ≥ 50% and leads the other by ≥ 20 points; "leaning" when one side has ≥ 40% and leads; otherwise "no clear signal".

Known weaknesses. One model only (more will be added). Countries smaller than a model grid cell (about 1°) use the nearest cell. Seasonal forecasts have real skill in the tropics during strong El Niño years, but limited skill in mid-latitudes such as Europe. Because the climate has warmed since 1993–2016, "warmer than normal" is the expected result almost everywhere.

Past El Niños

  1. ERA5 monthly reanalysis (C3S), 1979 to last year, 2 m temperature and precipitation, averaged to 1° and then to each country as above.
  2. Overlapping 3-month seasonal means for each year.
  3. The straight-line trend over all years is removed, so that warming alone does not make recent El Niños look hot.
  4. El Niño seasons (from the ONI episode list, including the current event) are compared with all other seasons: the average difference, and how many El Niño seasons were above the median.
  5. Signal rules: "usually wetter/warmer" when at least 70% of El Niño seasons were above the median; "usually drier/cooler" when at most 30% were; otherwise "no consistent pattern". Rainfall differences are shown as % of the long-term average.

Known weaknesses. Around 9–15 El Niño seasons per calendar season is a small sample. Country averages can hide opposite effects within a country (for example Peru's wetter north coast and drier southern highlands).

Air quality

Known weaknesses. A model forecast, not a measurement. Local sources (traffic, cooking, nearby fires) can make levels much higher or lower than the 40 km average.

Maps and borders

Country shapes come from Natural Earth (public domain). Borders and names imply no position on any dispute.

Change log