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      Unprecedented fire activity above the Arctic Circle linked to rising temperatures

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          Abstract

          Arctic fires can release large amounts of carbon from permafrost peatlands. Satellite observations reveal that fires burned ~4.7 million hectares in 2019 and 2020, accounting for 44% of the total burned area in the Siberian Arctic for the entire 1982–2020 period. The summer of 2020 was the warmest in four decades, with fires burning an unprecedentedly large area of carbon-rich soils. We show that factors of fire associated with temperature have increased in recent decades and identified a near-exponential relationship between these factors and annual burned area. Large fires in the Arctic are likely to recur with climatic warming before mid-century, because the temperature trend is reaching a threshold in which small increases in temperature are associated with exponential increases in the area burned.

          Getting burned

          Global warming is exacerbating the conditions that cause wildfires in many regions, including the Arctic, where extensive peatlands hold large amounts of carbon. However, is the extent of wildfires there increasing as would be expected given the changing conditions? Descals et al . found that during the summer of 2020, which was the warmest in four decades, Arctic fires burned an unprecedentedly large area of carbon-rich soils (see the Perspective by Post and Mack). They project that near-term climatic warming will cause an exponential increase in burned area in Arctic carbon-rich soils before mid-century. —HJS

          Abstract

          Global warming is creating conditions that will cause dramatic increases in Arctic wildfires.

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          Most cited references52

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          lavaan: AnRPackage for Structural Equation Modeling

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            Google Earth Engine: Planetary-scale geospatial analysis for everyone

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              Climate change and the permafrost carbon feedback.

              Large quantities of organic carbon are stored in frozen soils (permafrost) within Arctic and sub-Arctic regions. A warming climate can induce environmental changes that accelerate the microbial breakdown of organic carbon and the release of the greenhouse gases carbon dioxide and methane. This feedback can accelerate climate change, but the magnitude and timing of greenhouse gas emission from these regions and their impact on climate change remain uncertain. Here we find that current evidence suggests a gradual and prolonged release of greenhouse gas emissions in a warming climate and present a research strategy with which to target poorly understood aspects of permafrost carbon dynamics.
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                Author and article information

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                Journal
                Science
                Science
                American Association for the Advancement of Science (AAAS)
                0036-8075
                1095-9203
                November 04 2022
                November 04 2022
                : 378
                : 6619
                : 532-537
                Affiliations
                [1 ]CREAF, Centre de Recerca Ecològica i Aplicacions Forestals, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain.
                [2 ]CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, 08193 Barcelona, Catalonia, Spain.
                [3 ]TheTreeMap; Bagadou Bas, 46600 Martel, France.
                [4 ]CIDE, CSIC-UV-GV, 46113 València, Spain.
                [5 ]Forest Ecology and Forest Management Group, Wageningen University and Research, Wageningen, Netherlands.
                [6 ]Center for International Forestry Research (CIFOR), Bogor 16000, Indonesia.
                [7 ]Graduate School of Agriculture, Kyoto University, Kitashirakawa Oiwake-cho, Sakyo-ku, Kyoto 606-8502, Japan.
                Article
                10.1126/science.abn9768
                36378957
                031aed41-d764-4abd-ad5b-e7975e31f5f7
                © 2022
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