Global warming's brought more frequent, bigger and fiercer fires, which may make conditions even warmer

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Global warming has brought increasingly frequent and severe forest fires, and these may be increasing land surface warming, according to international scientists who analysed over a decade of satellite data from northern temperate and boreal forests and across Australia. They found a widespread warming effect one year after fires, and used mathematical simulations to calculate that bigger fires increased warming on land in North America, eastern boreal Asia and Australia. They found that plants released less water and reflected less heat following fires. However, the increase in warming over land after fires was not seen in parts of Siberia and eastern Europe. This may be due to the nature of the forests there, the authors say, which are mainly composed of deciduous broadleaf trees. Planting more broadleaf trees in fire-prone forests could potentially help curb any post-fire warming, they conclude.

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From: Springer Nature

Forest fire size may increase land warming

Increasing frequency and burn severity of forest fires may be increasing land surface warming, according to an analysis of over a decade of satellite data published in Nature. The findings highlight a previously overlooked factor that could affect future climate and fire dynamics.

Forest fires have become more frequent and larger, with some areas like the western USA and eastern Spain experiencing fire events that have doubled or tripled in size in recent decades. Larger forest fires typically result in greater loss of vegetation, but the effects of this increase of exposed land on the climate have not yet been established.

Chao Yue and colleagues analysed satellite data of wildfire events from 2003–2016 in northern temperate and boreal forests (40° N–70° N). They found a widespread warming effect one year after fire events—which is consistent with previous research—but, through a mathematical model, calculated that fire size amplified surface warming in North America and eastern boreal Asia. The analysis revealed that evapotranspiration and surface reflectivity decreased one year following a fire event—with greater decreases following larger fires—meaning that the surface was warming by releasing less water and absorbing more incoming radiation than previous years. Meanwhile, the amplified surface warming effect was not observed in western, central, and southeastern Siberia, and eastern Europe, which contain mixed forests and forests primarily composed of deciduous broadleaf trees.

The authors note that these trees may help moderate fire vulnerability and that future fire mitigation strategies could involve increasing the number of broadleaf trees in forests to weaken post-fire surface warming. However, further research is needed to assess how broadleaf trees may help suppress surface warming in Eurasian forests.

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Nature
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Organisation/s: Northwest A & F University, China
Funder: C.Y. was funded by the National Key Research and Development Program of China (2023YFB3907403), the National Science Foundation of China (U20A2090), the Second Tibetan Plateau Scientific Expedition and Research Program (2022QZKK0101) and the Strategic Priority Research Program of the Chinese Academy of Sciences (XDB40000000). S.L. was funded by Horizon 2020, HoliSoils (SEP-210673589) and Horizon Europe INFORMA (101060309).
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