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contributor authorBing Pu
contributor authorQinjian Jin
contributor authorPaul Ginoux
contributor authorYan Yu
date accessioned2023-04-12T18:44:30Z
date available2023-04-12T18:44:30Z
date copyright2022/12/01
date issued2022
identifier otherJCLI-D-21-0889.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4290162
description abstractCalifornia is one of the nation’s top agriculture producers and is vulnerable to extreme events such as droughts and heat waves. Concurrent extreme events may further stress water and energy resources, exerting greater adverse socioeconomic, environmental, and health impacts than individual events. Here we examine the features of compound drought, heat wave, and dust events in California during spring and summer. From 2003 to 2020, 16 compound events are found in warm seasons, with a mean duration of ∼4 days. Compound events are characterized by enhanced surface temperature up to 4.5°C over northern and western California, reduced soil moisture and vegetation density, and an increase in dust optical depth (DOD) by 0.05–0.1 over central and southern California. The enhanced DOD is largely associated with severe vegetation dieback that favors dust emissions and southeasterly wind anomalies that support northward transport of dust from source regions in southern California. Surface fine dust and PM
publisherAmerican Meteorological Society
titleCompound Heat Wave, Drought, and Dust Events in California
typeJournal Paper
journal volume35
journal issue24
journal titleJournal of Climate
identifier doi10.1175/JCLI-D-21-0889.1
journal fristpage4533
journal lastpage4552
page4533–4552
treeJournal of Climate:;2022:;volume( 035 ):;issue: 024
contenttypeFulltext


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