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contributor authorXiaodan Chen
contributor authorAiguo Dai
date accessioned2023-04-12T18:42:09Z
date available2023-04-12T18:42:09Z
date copyright2022/10/31
date issued2022
identifier otherJCLI-D-22-0023.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4290096
description abstractUnder increasing greenhouse gases, the Arctic warms about twice as fast as elsewhere, known as Arctic amplification (AA). AA weakens meridional temperature gradients and is hypothesized to weaken zonal wind and cause wavier circulation with stronger meridional wind (
publisherAmerican Meteorological Society
titleResponse of Meridional Wind to Greenhouse Gas Forcing, Arctic Sea-Ice Loss, and Arctic Amplification
typeJournal Paper
journal volume35
journal issue22
journal titleJournal of Climate
identifier doi10.1175/JCLI-D-22-0023.1
journal fristpage3675
journal lastpage3697
page3675–3697
treeJournal of Climate:;2022:;volume( 035 ):;issue: 022
contenttypeFulltext


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