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早期的融雪和极地喷气动力学共同影响了最近的西伯利亚极端火灾季节
Rebecca C Scholten1, Dim Coumou1,2, Fei Luo1,2
1Faculty of Science, Vrije Universiteit Amsterdam, Amsterdam, Netherlands.
概括
在西伯利亚,高温和早期融雪引发了前所未有的野火, 这些极端火灾正在向北移动, 加快了泥炭地的退化.
科学领域:
- 环境科学
- 气候科学
- 北极研究
背景情况:
- 西伯利亚东北部在2019-2021年夏季经历了前所未有的野火活动.
- 这些火灾发生在北极圈内的永久土,
研究的目的:
- 调查西伯利亚东北部极端火灾活动的气候驱动因素.
- 了解早期融雪,北极喷流行为和火灾发生之间的联系.
主要方法:
- 分析西伯利亚东北部的温度,融雪和闪电数据.
- 在过去的40年中对北极前喷流的发生和趋势的研究.
- 评估火灾活动及其空间分布,包括向北转移.
主要成果:
- 春季和夏季的高温被认为是火灾的主要原因.
- 自1966年以来,每十年的早融雪 (1.7天早) 和异常的北极前喷流导致了温暖干燥的条件.
- 在过去的40年里, 北极前喷气事件的频率增加了三倍以上,
- 燃烧显示向北移动, 影响碳丰富的永久土.
结论:
- 在西伯利亚东部, 气候因素相互关联,
- 观察到的火灾向北转移对碳丰富的永久土构成重大威胁.
- 这些泥炭地因火灾活动增加而加速退化,可能会对气候产生重大反.
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