Science1 publisher3 min readPublished
Extreme heat seasons stretched in opposite directions across half the world's land
A NASA Goddard team compared the 1980s with 2015 to 2024 and found extreme heat seasons growing at both ends, later in the western United States and earlier in western Europe, on schedules no summer calendar tracks.
The Scientist · Science desk

What happened
- Catherine Ivanovich of NASA's Goddard Institute for Space Studies and colleagues report in AGU Advances that extreme heat events have grown more frequent in the months before and after the traditional warm season.
- Extreme heat seasons expanded significantly over just over half the world's land area when measured as dry heat, and just under half when measured as humid heat stress.
- The fastest growth came in the two months after the historical heat season in the western United States, eastern China, northern Africa and eastern Europe, and in the two months before it in western Europe, southern Africa and northwestern India.
- Phoenix recorded 183 extreme heat days by temperature in the 1980s baseline decade and 338 in the decade ending in 2024.
- In March, after the study period closed, Phoenix had nine days above 100 F, a March the historical record contains only one precedent for.
Compiled by The ScientistSomething wrong?How this is made
Why it matters
- decision A city choosing between a thermometer threshold and a heat-stress index is choosing which shoulder season to staff for, because in Phoenix those two measures drifted in opposite directions.
- constraint A heat calendar borrowed from another region can now be wrong at both ends, which is a harder problem to fix than adding July capacity.
- exposure The people newly reachable are the ones outdoors in the weeks flanking the recognised season, when neither their physiology nor the alert system has caught up.
- contradiction The authors' own prior, that warming lowers the bar to dangerous heat evenly across the year, failed, so planning drawn from global mean warming will misread local timing.
The sharpest number in this paper sits inside one city and points two ways at once. Phoenix's dry-heat extremes now have a median date 10 days later in the year than in the 1980s, while its humid-heat extremes have a median 5.5 days earlier [10]. The first measure is a plain thermometer reading. The second is wet-bulb globe temperature, which folds humidity and solar radiation in with air temperature to approximate the heat load a body has to shed [4]. Which of the two a jurisdiction writes its alert trigger on decides which end of its calendar it prepares for.
Extremes here are defined relatively, as days in the hottest 5% of the daily record, counted once in the baseline decade and again in the recent one [3]. That is a deliberately low-tech definition, and it is what gives the two-month windows on either side of each region's historical heat season something stable to be measured against [6]. The team also ran the analysis on two datasets, NASA's and the European Centre for Medium-Range Weather Forecasts', which is the control that matters most when the underlying product is a reanalysis rather than a station record, and the pattern largely held [15]. Averages had already been mapped: midlatitude summer conditions have lengthened by roughly six days per decade since 1990, but individual extreme events need not move in step with the seasonal mean [19].
Phoenix's count grew by 155 days between the two decades, an increase of 85% [21]. The more useful split is where they fell. None of the 1980s extremes landed after the heat season had ended; 6% of the 2015 to 2024 ones did [9], which works out to about 20 days across that decade, roughly two a year [22]. Small in count, and the acclimation argument is what makes it worth attention: the same temperature is harder on a body that has not had weeks to adjust, and harder again after months of enduring it, which is the sense in which a summer cooling-center schedule is mistimed rather than merely undersized [18]. That acclimation argument sits outside the study's method, which only counts days [3]. The 2024 tail was visible regardless, with 113 consecutive days above 100 F and then, from late September into mid-October, 21 straight days tying or breaking daily records [11].
The county mortality figures invite a causal read they cannot carry. July held 64% of Maricopa County's 645 heat-related deaths in 2023 and 46% of 608 in 2024 [13][12], so deaths outside July rose from roughly 232 to roughly 328 even as the annual total fell [23]. Two years is a distribution, not a trend, and one hot July can move that split by itself. The paper's data are heat days, counted independent of mortality [3].
Ivanovich and her coauthors, Benjamin Cook at GISS and Sonali Shukla McDermid at New York University, went in expecting warming to make dangerous thresholds uniformly easier to cross all year, and that is not what came out [2][16]. Ivanovich puts the result no higher than a compelling first line of evidence, on the grounds that extreme heat is rare by definition and out-of-season extreme heat rarer still [17]. So the work maps which direction each region's heat season is drifting, leaving the calendar dates for switching a heat plan on and off as the next open question.
What to watch
- Whether Phoenix's nine 100 F days in March register as a spring signal once the record is extended past the 2024 cutoff.
- Whether Maricopa County's monthly death breakdown keeps moving out of July over more years than the two now on the table.
- Whether any jurisdiction moves its alert start and end dates off the summer calendar, and which heat metric it uses to set them.