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contributor authorJesse Norris
contributor authorAlex Hall
contributor authorChad W. Thackeray
contributor authorDi Chen
contributor authorGavin D. Madakumbura
date accessioned2023-04-12T18:41:08Z
date available2023-04-12T18:41:08Z
date copyright2022/10/14
date issued2022
identifier otherJCLI-D-21-0842.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4290068
description abstractLarge uncertainty exists in hydrologic sensitivity (HS), the global-mean precipitation increase per degree of warming, across global climate model (GCM) ensembles. Meanwhile, the global circulation and hence global precipitation are sensitive to variations of surface temperature under internal variability. El Niño–Southern Oscillation (ENSO) is the most dominant mode of global temperature variability and hence of precipitation variability. Here we show in phase 6 of the Coupled Model Intercomparison Project (CMIP6) that the strength of HS under ENSO is predictive of HS in the climate change context (
publisherAmerican Meteorological Society
titleEvaluating Hydrologic Sensitivity in CMIP6 Models: Anthropogenic Forcing versus ENSO
typeJournal Paper
journal volume35
journal issue21
journal titleJournal of Climate
identifier doi10.1175/JCLI-D-21-0842.1
journal fristpage3355
journal lastpage3368
page3355–3368
treeJournal of Climate:;2022:;volume( 035 ):;issue: 021
contenttypeFulltext


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