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In the Arctic, consequences of heat waves linger

In the Arctic, consequences of heat waves linger
Heat wave area groups within the study domain >50°N, 40–180°E divided by z-scores of AirTanomaly (ERA5 reanalysis) during 1979–2019. “noHW”: z-scores of AirTanomaly less than 2 during q1 and q2 in 2020; “Q1”: z-scores greater than 2 during q1 in 2020; “Q2”: z-scores greater than 2 during q2 in 2020; “Q1,Q2”: z-scores greater than 2 during q1 and q2 in 2020. Credit: Global Biogeochemical Cycles (2025). DOI: 10.1029/2025GB008607

Throughout the first half of 2020, average monthly temperatures in Siberia reached 6°C above the norm. The situation climaxed on 20 June, when the temperature in the town of Verkhoyansk climbed to 38°C (100.4°F), the highest temperature ever recorded north of the Arctic Circle. With the extreme heat came wildfires, insect outbreaks, and thawing permafrost.

Now Kwon and team suggest that the effects of the 2020 heat wave were still detectable the following year in the form of warmer- and wetter-than-usual soils. The findings are published in the journal Global Biogeochemical Cycles.

The researchers obtained data on temperatures, precipitation, and other climatic factors from the European Centre for Medium-Range Weather Forecasts and incorporated them into a model of high-latitude ecosystems. To capture the effect of the 2020 Siberian heat wave, they replaced data from 2020 with data from each of the previous 5 years (2015 to 2019), which provided five estimates of what regional ecosystems might have looked like in 2021 had the heat wave not occurred.

The analysis indicated that the caused to remain roughly 1.2°C, or about 150%, warmer in 2021 than it would have been without the heat wave, even though air temperatures had returned to normal. The also melted soil ice, resulting in wetter soil than usual. Root zone soil water availability, a measure of how much water soil can hold in the rooting depth of plants, increased by 10.9% in forests in 2021 and by 9.3% in grasslands. However, some of this meltwater left the soil via runoff.

In response to warmer, wetter soil, microbes proliferated and caused the soil ecosystem to emit more than usual, the modeling indicated. In forests, this effect was largely offset by an increase in photosynthesis as plants flourished under the new conditions. In grasslands, on the other hand, photosynthesis initially increased during the heat wave event but then quickly decreased until 2021 as plants used up the available water and died off.

As a result of the 2020 , the researchers reported, forests gained an additional 6 grams of carbon per square meter in the first half of 2021, whereas grasslands lost 10.9 grams of carbon per square meter.

More information:
Min Jung Kwon et al, Legacy Effects of the Siberian Heatwave of 2020 on Above‐ and Belowground Processes, Global Biogeochemical Cycles (2025). DOI: 10.1029/2025GB008607

This story is republished courtesy of Eos, hosted by the American Geophysical Union. Read the original story here.

Citation:
In the Arctic, consequences of heat waves linger (2025, August 25)
retrieved 25 August 2025
from https://phys.org/news/2025-08-arctic-consequences-linger.html

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