The October–December tie hurdle for 2026 is 1.02–1.03°C above 1991–2020, compared with the 2023 historical maximum of 0.85°C. The difference, 0.17–0.18°C, compares equal-month and day-weighted averaging.

For 2026 to overtake 2024 in this calculation, October–December would have to exceed a tie hurdle of 1.02–1.03°C above 1991–2020. That is 0.17–0.18°C above the warmest previous final quarter in the ERA5 monthly record.

The ranges compare two ways of averaging: giving each month equal weight, or weighting it by its number of days. They show sensitivity to that choice, not physical uncertainty. A new record requires exceeding the unrounded hurdle; reaching the rounded label does not settle the comparison.

The Copernicus Climate Change Service's September bulletin, released in October, supplies the timely question. It puts 2026 second for January–September and says a repeat of late 2023 would bring it close to 2024. The hurdle calculation gives that comparison a historical scale.

These are global surface air temperature anomalies from C3S/ECMWF's ERA5 series, with observations through September 2026. Each month is compared with its own 1991–2020 average. A high anomaly means warmth relative to the same time of year; it does not mean the closing months must be the hottest months in absolute temperature. This is global air temperature across land and ocean, rather than local weather or sea surface temperature.

The highest previous October–December anomaly was 0.85°C in 2023. Matching that final quarter would be insufficient because the annual average also carries the earlier months. January–September 2026 averaged 0.62°C, behind 2024's 0.70–0.71°C. The remaining quarter must offset that accumulated deficit as well as match the annual benchmark.

Cumulative anomalies for 2024 and 2026. January–September 2026 is second at 0.62°C, versus first-place 2024 at 0.70–0.71°C. If October–December repeats 2023, 2026 ends at 0.67–0.68°C, less than 0.05°C below 2024's 0.72°C. Shading is hypothetical for 2026 only; 2024 remains actual.

Yet the repeat scenario would leave only a small annual gap: 0.67–0.68°C for 2026, compared with 0.72°C for 2024, a difference of less than 0.05°C. C3S's “close to” comparison is consistent with this result. Second through September is already a warm year in this record.

A historical maximum is a comparison, not a ceiling. C3S also reports strengthening El Niño conditions; these anomaly calculations do not test that outlook or assign a probability to a new annual record. Nor does a single year's ranking measure the Paris Agreement's long-term warming level.

Friction notes

  • No exempt data numbers: the prose's temperature values, comparison years and baseline appear on the charts.
  • Independent final editorial review is approved; the author's personal voice pass remains outstanding.

How this was made

The frozen monthly data, provenance and licence, calculation and chart builder reproduce the numbers. Both averaging choices use the supplied anomalies and actual calendars. This is a conditional calculation on that snapshot, rather than a reproduction of C3S's eventual annual classification. From the stories folder, run:

python3 2026-temperature-record-src/calculate.py
npm ci
node 2026-temperature-record-make-charts.mjs
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