Quantifying the influence of global warming on unprecedented extreme climate events

被引:609
作者
Diffenbaugh, Noah S. [1 ,2 ]
Singh, Deepti [1 ,3 ]
Mankin, Justin S. [1 ,3 ,4 ,5 ]
Horton, Daniel E. [1 ,6 ]
Swain, Daniel L. [1 ,7 ]
Touma, Danielle [1 ]
Charland, Allison [1 ]
Liu, Yunjie [1 ]
Haugen, Matz [1 ]
Tsiang, Michael [1 ,8 ]
Rajaratnam, Bala [1 ,2 ,9 ]
机构
[1] Stanford Univ, Dept Earth Syst Sci, Stanford, CA 94305 USA
[2] Stanford Univ, Woods Inst Environm, Stanford, CA 94305 USA
[3] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
[4] Stanford Univ, Emmett Interdisciplinary Program Environm & Resou, Stanford, CA 94305 USA
[5] NASA, Goddard Inst Space Studies, New York, NY 10025 USA
[6] Northwestern Univ, Dept Earth & Planetary Sci, Evanston, IL 60208 USA
[7] Univ Calif Los Angeles, Inst Environm & Sustainabil, Los Angeles, CA 90095 USA
[8] Univ Calif Los Angeles, Dept Stat, Los Angeles, CA 90095 USA
[9] Stanford Univ, Dept Stat, Stanford, CA 94305 USA
基金
美国国家科学基金会; 美国国家卫生研究院;
关键词
event attribution; climate extremes; climate change; global warming; ANTHROPOGENIC CONTRIBUTION; ATTRIBUTION; TEMPERATURE; PRECIPITATION; WEATHER; VARIABILITY; DROUGHT; CONTEXT; CMIP5; HEAT;
D O I
10.1073/pnas.1618082114
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
070301 [无机化学]; 070403 [天体物理学]; 070507 [自然资源与国土空间规划学]; 090105 [作物生产系统与生态工程];
摘要
Efforts to understand the influence of historical global warming on individual extreme climate events have increased over the past decade. However, despite substantial progress, events that are unprecedented in the local observational record remain a persistent challenge. Leveraging observations and a large climate model ensemble, we quantify uncertainty in the influence of global warming on the severity and probability of the historically hottest month, hottest day, driest year, and wettest 5-d period for different areas of the globe. We find that historical warming has increased the severity and probability of the hottest month and hottest day of the year at > 80% of the available observational area. Our framework also suggests that the historical climate forcing has increased the probability of the driest year andwettest 5-d period at 57% and 41% of the observed area, respectively, although we note important caveats. For the most protracted hot and dry events, the strongest and most widespread contributions of anthropogenic climate forcing occur in the tropics, including increases in probability of at least a factor of 4 for the hottest month and at least a factor of 2 for the driest year. We also demonstrate the ability of our framework to systematically evaluate the role of dynamic and thermodynamic factors such as atmospheric circulation patterns and atmospheric water vapor, and find extremely high statistical confidence that anthropogenic forcing increased the probability of record-low Arctic sea ice extent.
引用
收藏
页码:4881 / 4886
页数:6
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