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在全球变暖的情况下,极端降水的频率随着事件的罕见性而广泛增加。

Frequency of extreme precipitation increases extensively with event rareness under global warming.

机构信息

CICERO Center for International Climate Research - Oslo, 0318, Oslo, Norway.

Institute for Atmospheric and Climate Science, ETH Zurich, 8092, Zurich, Switzerland.

出版信息

Sci Rep. 2019 Nov 5;9(1):16063. doi: 10.1038/s41598-019-52277-4.

Abstract

The intensity of the heaviest extreme precipitation events is known to increase with global warming. How often such events occur in a warmer world is however less well established, and the combined effect of changes in frequency and intensity on the total amount of rain falling as extreme precipitation is much less explored, in spite of potentially large societal impacts. Here, we employ observations and climate model simulations to document strong increases in the frequencies of extreme precipitation events occurring on decadal timescales. Based on observations we find that the total precipitation from these intense events almost doubles per degree of warming, mainly due to changes in frequency, while the intensity changes are relatively weak, in accordance to previous studies. This shift towards stronger total precipitation from extreme events is seen in observations and climate models, and increases with the strength - and hence the rareness - of the event. Based on these results, we project that if historical trends continue, the most intense precipitation events observed today are likely to almost double in occurrence for each degree of further global warming. Changes to extreme precipitation of this magnitude are dramatically stronger than the more widely communicated changes to global mean precipitation.

摘要

已知随着全球变暖,最强极端降水事件的强度会增加。然而,在一个更温暖的世界中,此类事件发生的频率是不太确定的,而且降水强度和频率的变化对极端降水总量的综合影响,尽管可能会产生巨大的社会影响,但仍未得到充分探索。在这里,我们利用观测资料和气候模式模拟来记录极端降水事件在数十年时间尺度上发生的频率的强烈增加。基于观测结果,我们发现,这些强烈事件的总降水量每升温 1 度几乎增加一倍,这主要是由于频率的变化,而强度变化相对较弱,这与之前的研究一致。这种极端事件导致的总降水量的变化趋势在观测和气候模型中都得到了体现,并且随着事件的强度——因此也随着事件的罕见性——而增加。基于这些结果,我们预测如果历史趋势继续下去,那么今天观测到的最强烈的降水事件,在未来每升温 1 度,其发生的可能性就会增加近一倍。这种极端降水的变化幅度比更广泛传播的全球平均降水变化幅度大得多。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/593f/6831572/4c6cf8b38c7c/41598_2019_52277_Fig1_HTML.jpg

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