北极振荡的增加解释了俄罗斯野火的大部分年际变化

IF 2.7 3区 农林科学 Q2 ECOLOGY
Andrei G. Lapenis, Leonid N. Yurganov
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引用次数: 0

摘要

在过去二十年中,北半球北方野火造成的温室气体排放不断增加,引起了人们的极大关注,突显了2021年前所未有的野火季节。我们的计算表明,在2002年至2020年期间,俄罗斯的野火释放了大约726±280 Tg CO 2eqv yr - 1。这与从遥感数据得出的类似估计值密切一致,远远超过俄罗斯国家清单报告(NIR)中发现的较早的近似值,高出2至3倍。值得注意的是,仅在2021年,俄罗斯的野火就排放了异常高的1,700 Tg CO 2eqv,超过了该国化石燃料消耗的碳排放量。因此,这种情况导致俄罗斯森林的碳吸收几乎完全平衡。我们的分析将2002年至2021年间野火频率变化的50%以上归因于北极涛动(AO)的变化。这表明有可能利用AO作为野火的预测变量。值得注意的是,AO本身受到北极海冰持续消退的影响。由此可以推断,在可预见的未来,俄罗斯森林可能经历从碳汇角色向大气碳的潜在净贡献者的转变。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Increase in Arctic Oscillations explains most interannual variability in Russia’s wildfires
Over the past two decades, the escalating emissions of greenhouse gases from boreal wildfires in the Northern Hemisphere have drawn significant attention, underscoring an unprecedented wildfire season in 2021. Our calculations indicate that between 2002 and 2020, wildfires in Russia released approximately 726 ± 280 Tg CO 2eqv yr −1 . This aligns closely with similar estimates derived from remote sensing data, far surpassing the earlier approximations found in the Russian National Inventory Report (NIR) by a factor of 2 to 3. Notably, in 2021 alone, Russia’s wildfires emitted an exceptionally high amount of 1,700 Tg CO 2eqv , exceeding the carbon emissions from the country’s fossil fuel consumption. Consequently, this situation led to an almost complete counterbalance of carbon assimilation by Russian forests. Our analysis attributes over 50% of the variation in wildfire frequency between 2002 and 2021 to shifts in the Arctic Oscillation (AO). This suggests a potential for utilizing AO as a predictive variable for wildfires. It’s noteworthy that the AO itself is influenced by the sustained regression of Arctic sea-ice. From this, it can be inferred that in the foreseeable future, Russian forests might undergo a transition from their role as carbon sinks to the potential net contributors of carbon to the atmosphere.
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来源期刊
CiteScore
4.50
自引率
6.20%
发文量
256
审稿时长
12 weeks
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