The Role of Anthropogenic Forcing in Western United States Hydroclimate Extremes

被引:4
|
作者
Zhang, Wei [1 ]
Gillies, Robert [1 ,2 ]
机构
[1] Utah State Univ, Dept Plants Soils & Climate, Logan, UT 84322 USA
[2] Utah State Univ, Utah Climate Ctr, Logan, UT USA
基金
美国国家科学基金会;
关键词
western U; S; precipitation roller coaster; hydroclimatic intensity; anthropogenic forcing; HYDROLOGICAL CYCLE; CLIMATE; PRECIPITATION; INTENSITY; DROUGHT; EVENTS;
D O I
10.1029/2022GL100659
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Despite lower-than-average total precipitation in the western states of the U.S., the 2021 "precipitation roller coaster" defined as large precipitation swings has pointed to a strong hydroclimatic intensity (HYINT). Here we examine the 2021 HYINT using an index-a product of the average precipitation intensity (INT) and dry spell length (DSL). HYINT exhibited an extremely high value in the western U.S. in 2021. INT and DSL contribute differently to the 2021 HYINT, with large spatial variability. Overall, the 2021 extreme HYINT in central California and Utah is tied more to large INT, than to DSL. Meanwhile, the historical trends in INT and DSL may have contributed to the extreme 2021 HYINT event. The fraction of attributable risk framework reveals that the 2021 extreme HYINT is more likely to occur with anthropogenic forcing (e.g., 7.3 times more likely for HYINT exceeding 1.3) than natural forcing alone.
引用
收藏
页数:8
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