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快速升温导致澳大利亚东北部野火频发。

Rapid warming has resulted in more wildfires in northeastern Australia.

机构信息

State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China; University of Chinese Academy of Sciences, Beijing 100049, China.

State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China; CAS Center for Excellence in Quaternary Science and Global Change, Xi'an 710061, China; Qingdao National Laboratory for Marine Science and Technology, Qingdao, China.

出版信息

Sci Total Environ. 2021 Jun 1;771:144888. doi: 10.1016/j.scitotenv.2020.144888. Epub 2021 Jan 29.

Abstract

Wildfires, or bushfires, are one of the most destructive natural disasters in Australia, which can cause many deaths of stock, native animals, sometimes humans, and huge impacts on infrastructure. Reconstructing past wildfires and exploring the links between wildfires and climate are essential for understanding the dynamics of wildfires and for predicting future risks. In this study, the frequency of wildfires in northeastern Australia over the past 25,000 years was reconstructed from the charcoal records preserved in peat and lake sediments. The results showed that the frequency of wildfires were relatively low during the cool last glacial period and the warm mid Holocene, indicating that the stable mean climate conditions, whether cool or warm, would not independently initiate increased wildfires in northeastern Australia. The most frequent wildfires occurred during the last deglaciation period, when Earth's climate warmed and the warming rate was the highest over the last 25,000 years, before recent anthropogenic warming. It suggested that the rapid global warming may greatly increase the likelihood of dangerous wildfires in northeastern Australia during the last deglaciation. The wildfires reactivated over the most recent 4000 years, coinciding with amplified climate variability and probably an expansion of human activity. The rapid warming of global climate during the last deglaciation period is an ideal analogue for current anthropogenic global warming. The comparison between fire count and temperature changes in Australia since 2003 also showed that the fire frequency in Australia in recent years is more closely correlated with the warming amplitude, rather than mean temperature. Our results implied that the wildfire risk in northeastern Australia may increase further under the expected accelerating global warming, if human management systems does not intrude. Wildfire modeling could benefit greatly by considering the relationship of fires with climate variability rather than only with stable climate scenarios.

摘要

野火,又称丛林大火,是澳大利亚最具破坏性的自然灾害之一,它可能导致大量牲畜、本地动物死亡,有时还会导致人类死亡,并对基础设施造成巨大影响。重建过去的野火事件并探索野火与气候之间的联系,对于理解野火的动态以及预测未来的风险至关重要。在这项研究中,从保存在泥炭和湖泊沉积物中的木炭记录中重建了过去 25000 年来澳大利亚东北部野火的发生频率。结果表明,在寒冷的末次冰期和温暖的中全新世,野火的发生频率相对较低,这表明无论是寒冷还是温暖,稳定的平均气候条件不会独立引发澳大利亚东北部野火的增加。最频繁的野火发生在末次冰消期,当时地球气候变暖,变暖速度是过去 25000 年来最高的,而最近的人为变暖还没有发生。这表明,快速的全球变暖可能会大大增加澳大利亚东北部在末次冰消期发生危险野火的可能性。最近 4000 年来,野火再次活跃,与气候变率的放大和人类活动的扩张相吻合。末次冰消期全球气候的快速变暖是当前人为全球变暖的理想类比。自 2003 年以来,澳大利亚火灾次数与温度变化的比较也表明,近年来澳大利亚的火灾频率与变暖幅度的相关性更密切,而不是与平均温度的相关性更密切。如果人类管理系统不干预,我们的研究结果表明,在预期的加速全球变暖的情况下,澳大利亚东北部的野火风险可能会进一步增加。野火模型通过考虑火灾与气候变率的关系而不仅仅是与稳定气候情景的关系,将大大受益。

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