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Kang, Sarah M.
Climate Dynamics Lab
Research Interests
  • Climate change, ITCZ, Atmospheric general circulation, Polar amplification


Modeling evidence that ozone depletion has impacted extreme precipitation in the austral summer

DC Field Value Language Kang, Sarah M. ko Polvani, L.M. ko Fyfe, J.C. ko Son, S.-W. ko Sigmond, M. ko Correa, G.J.P. ko 2014-04-14T00:27:37Z - 2013-08-30 ko 2013-08 ko
dc.identifier.citation GEOPHYSICAL RESEARCH LETTERS, v.40, no.15, pp.4054 - 4059 ko
dc.identifier.issn 0094-8276 ko
dc.identifier.uri -
dc.description.abstract The impacts of stratospheric ozone depletion on the extremes of daily precipitation in the austral summer are explored using two global climate models. Both models indicate that stratospheric ozone losses since the late 1970s may have increased the frequency and intensity of very heavy precipitation in austral summer over southern high and subtropical latitudes, and may have decreased the frequency and intensity over southern midlatitudes. This hemispheric wide pattern of extreme precipitation response projects strongly onto a previously identified pattern of seasonal mean precipitation response, both of which are shown to be likely of dynamic rather than thermodynamic origin. Key Points: Ozone depletion has an impact on extreme rainfall in the Southern Hemisphere. Ozone depletion induced extreme rainfall change has a geographical pattern. The extreme rainfall changes caused by ozone depletion is of dynamic origin. ko
dc.description.statementofresponsibility close -
dc.language 영어 ko
dc.title Modeling evidence that ozone depletion has impacted extreme precipitation in the austral summer ko
dc.type ARTICLE ko
dc.identifier.scopusid 2-s2.0-84881272970 ko
dc.identifier.wosid 000323660000050 ko
dc.type.rims ART ko
dc.description.wostc 5 *
dc.description.scopustc 3 * 2015-02-28 * 2014-07-12 *
dc.identifier.doi 10.1002/grl.50769 ko
dc.identifier.url ko
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