Climate warming increases extreme daily wildfire growth risk in California

被引:57
作者
Brown, Patrick T. [1 ,2 ,3 ]
Hanley, Holt [2 ,4 ,5 ]
Mahesh, Ankur [6 ,7 ]
Reed, Colorado [8 ]
Strenfel, Scott J. [9 ]
Davis, Steven J. [10 ]
Kochanski, Adam K. [2 ,4 ]
Clements, Craig B. [2 ,4 ]
机构
[1] Breakthrough Inst, Climate & Energy Team, Berkeley, CA 94704 USA
[2] San Jose State Univ, Wildfire Interdisciplinary Res Ctr WIRC, San Jose, CA 95192 USA
[3] Johns Hopkins Univ, Energy Policy & Climate Program, Baltimore, MD 21205 USA
[4] San Jose State Univ, Dept Meteorol & Climate Sci, San Jose, CA USA
[5] KSBW News, Salinas, CA USA
[6] Lawrence Berkeley Natl Lab, Climate & EcoSyst Sciences Div, Berkeley, CA USA
[7] Univ Calif Berkeley, Earth & Planetary Sci, Berkeley, CA USA
[8] Univ Calif Berkeley, Dept Elect Engn & Comp Sci, Berkeley, CA USA
[9] Pacific Gas & Elect Co, Oakland, CA USA
[10] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA USA
基金
美国国家科学基金会;
关键词
ATTRIBUTION; IMPACTS; WEATHER; MODEL;
D O I
10.1038/s41586-023-06444-3
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
07 ; 0710 ; 09 ;
摘要
California has experienced enhanced extreme wildfire behaviour in recent years1-3, leading to substantial loss of life and property4,5. Some portion of the change in wildfire behaviour is attributable to anthropogenic climate warming, but formally quantifying this contribution is difficult because of numerous confounding factors6,7 and because wildfires are below the grid scale of global climate models. Here we use machine learning to quantify empirical relationships between temperature (as well as the influence of temperature on aridity) and the risk of extreme daily wildfire growth (>10,000 acres) in California and find that the influence of temperature on the risk is primarily mediated through its influence on fuel moisture. We use the uncovered relationships to estimate the changes in extreme daily wildfire growth risk under anthropogenic warming by subjecting historical fires from 2003 to 2020 to differing background climatological temperatures and aridity conditions. We find that the influence of anthropogenic warming on the risk of extreme daily wildfire growth varies appreciably on a fire-by-fire and day-by-day basis, depending on whether or not climate warming pushes conditions over certain thresholds of aridity, such as 1.5 kPa of vapour-pressure deficit and 10% dead fuel moisture. So far, anthropogenic warming has enhanced the aggregate expected frequency of extreme daily wildfire growth by 25% (5-95 range of 14-36%), on average, relative to preindustrial conditions. But for some fires, there was approximately no change, and for other fires, the enhancement has been as much as 461%. When historical fires are subjected to a range of projected end-of-century conditions, the aggregate expected frequency of extreme daily wildfire growth events increases by 59% (5-95 range of 47-71%) under a low SSP1-2.6 emissions scenario compared with an increase of 172% (5-95 range of 156-188%) under a very high SSP5-8.5 emissions scenario, relative to preindustrial conditions.
引用
收藏
页码:760 / +
页数:8
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