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Lee, Myong-In
UNIST Climate Environment Modeling Lab.
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dc.citation.endPage 2937 -
dc.citation.number 12 -
dc.citation.startPage 2919 -
dc.citation.title JOURNAL OF CLIMATE -
dc.citation.volume 21 -
dc.contributor.author Lin, Jia-Lin -
dc.contributor.author Mapes, Brian E. -
dc.contributor.author Weickmann, Klaus M. -
dc.contributor.author Kiladis, George N. -
dc.contributor.author Schubert, Siegfried D. -
dc.contributor.author Suarez, Max J. -
dc.contributor.author Bacmeister, Julio T. -
dc.contributor.author Lee, Myong-In -
dc.date.accessioned 2023-12-22T08:39:40Z -
dc.date.available 2023-12-22T08:39:40Z -
dc.date.created 2014-10-31 -
dc.date.issued 2008-06 -
dc.description.abstract This study evaluates the fidelity of North American monsoon and associated intraseasonal variability in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) coupled general circulation models (CGCMs). Twenty years of monthly precipitation data from each of the 22 models' twentieth-century climate simulations, together with the available daily precipitation data from 12 of them, are analyzed and compared with Global Precipitation Climatology Project (GPCP) monthly and daily precipitation. The authors focus on the seasonal cycle and horizontal pattern of monsoon precipitation in conjunction with the two dominant convectively coupled equatorial wave modes: the eastward-propagating Madden-Julian oscillation (MJO) and the westward-propagating easterly waves.

The results show that the IPCC AR4 CGCMs have significant problems and display a wide range of skill in simulating the North American monsoon and associated intraseasonal variability. Most of the models reproduce the monsoon rainbelt, extending from southeast to northwest, and its gradual northward shift in early summer, but overestimate the precipitation over the core monsoon region throughout the seasonal cycle and fail to reproduce the monsoon retreat in the fall. Additionally, most models simulate good westward propagation of the easterly waves, but relatively poor eastward propagation of the MJO and overly weak variances for both the easterly waves and the MJO. There is a tendency for models without undiluted updrafts in their deep convection scheme to produce better MJO propagation.
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dc.identifier.bibliographicCitation JOURNAL OF CLIMATE, v.21, no.12, pp.2919 - 2937 -
dc.identifier.doi 10.1175/2007JCLI1815.1 -
dc.identifier.issn 0894-8755 -
dc.identifier.scopusid 2-s2.0-48749104280 -
dc.identifier.uri https://scholarworks.unist.ac.kr/handle/201301/8120 -
dc.identifier.url http://www.scopus.com/inward/record.url?partnerID=HzOxMe3b&scp=48749104280 -
dc.identifier.wosid 000257246700012 -
dc.language 영어 -
dc.publisher AMER METEOROLOGICAL SOC -
dc.title North American monsoon and convectively coupled equatorial waves simulated by IPCC AR4 coupled GCMs -
dc.type Article -
dc.description.journalRegisteredClass scopus -
dc.subject.keywordPlus GENERAL-CIRCULATION MODEL -
dc.subject.keywordPlus GULF-OF-CALIFORNIA -
dc.subject.keywordPlus SIMPLE MULTICLOUD
PARAMETERIZATION
-
dc.subject.keywordPlus PACIFIC TROPICAL CYCLOGENESIS -
dc.subject.keywordPlus SURFACE TEMPERATURE
ANOMALIES
-
dc.subject.keywordPlus MADDEN-JULIAN OSCILLATION -
dc.subject.keywordPlus LARGE-SCALE MODELS -
dc.subject.keywordPlus EASTERLY
WAVES
-
dc.subject.keywordPlus PART I -
dc.subject.keywordPlus CUMULUS PARAMETERIZATION -

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