Attribution of climate extreme events

被引:0
|
作者
Trenberth K.E. [1 ]
Fasullo J.T. [1 ]
Shepherd T.G. [2 ]
机构
[1] National Center for Atmospheric Research (NCAR), PO Box 3000, Boulder, 80307, CO
[2] Department of Meteorology, University of Reading, Reading
基金
美国国家科学基金会;
关键词
D O I
10.1038/nclimate2657
中图分类号
学科分类号
摘要
There is a tremendous desire to attribute causes to weather and climate events that is often challenging from a physical standpoint. Headlines attributing an event solely to either human-induced climate change or natural variability can be misleading when both are invariably in play. The conventional attribution framework struggles with dynamically driven extremes because of the small signal-to-noise ratios and often uncertain nature of the forced changes. Here, we suggest that a different framing is desirable, which asks why such extremes unfold the way they do. Specifically, we suggest that it is more useful to regard the extreme circulation regime or weather event as being largely unaffected by climate change, and question whether known changes in the climate system's thermodynamic state affected the impact of the particular event. Some examples briefly illustrated include 'snowmaggedon' in February 2010, superstorm Sandy in October 2012 and supertyphoon Haiyan in November 2013, and, in more detail, the Boulder floods of September 2013, all of which were influenced by high sea surface temperatures that had a discernible human component. © 2015 Macmillan Publishers Limited.
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页码:725 / 730
页数:5
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