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Lee, Myong-In
UNIST Climate Environment Modeling Lab.
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dc.citation.endPage 534 -
dc.citation.number 1-2 -
dc.citation.startPage 517 -
dc.citation.title CLIMATE DYNAMICS -
dc.citation.volume 43 -
dc.contributor.author Kim, Daehyun -
dc.contributor.author Lee, Myong-In -
dc.contributor.author Kim, Dongmin -
dc.contributor.author Schubert, Siegfried D. -
dc.contributor.author Waliser, Duane E. -
dc.contributor.author Tian, Baijun -
dc.date.accessioned 2023-12-22T02:37:26Z -
dc.date.available 2023-12-22T02:37:26Z -
dc.date.created 2013-08-28 -
dc.date.issued 2014-07 -
dc.description.abstract Tropical subseasonal variability of precipitation from five global reanalyses (RAs) is evaluated against Global Precipitation Climatology Project (GPCP) and Tropical Rainfall Measuring Mission (TRMM) observations. The RAs include the three generations of global RAs from the National Center for Environmental Prediction (NCEP), and two other RAs from the European Centre for Medium-Range Weather Forecasts (ECMWF) and the National Aeronautics and Space Administration/Goddard Space Flight Center (NASA/GSFC). The analysis includes comparisons of the seasonal means and subseasonal variances of precipitation, and probability densities of rain intensity in selected areas. In addition, the space-time power spectrum was computed to examine the tropical Madden-Julian Oscillation (MJO) and convectively coupled equatorial waves (CCEWs). The modern RAs show significant improvement in their representation of the mean state and subseasonal variability of precipitation when compared to the two older NCEP RAs: patterns of the seasonal mean state and the amplitude of subseasonal variability are more realistic in the modern RAs. However, the probability density of rain intensity in the modern RAs show discrepancies from observations that are similar to what the old RAs have. The modern RAs show higher coherence of CCEWs with observed variability and more realistic eastward propagation of the MJO precipitation. The modern RAs, however, exhibit common systematic deficiencies including: (1) variability of the CCEWs that tends to be either too weak or too strong, (2) limited coherence with observations for waves other than the MJO, and (3) a systematic phase lead or lag for the higher-frequency waves. -
dc.identifier.bibliographicCitation CLIMATE DYNAMICS, v.43, no.1-2, pp.517 - 534 -
dc.identifier.doi 10.1007/s00382-013-1890-x -
dc.identifier.issn 0930-7575 -
dc.identifier.scopusid 2-s2.0-84906088054 -
dc.identifier.uri https://scholarworks.unist.ac.kr/handle/201301/4028 -
dc.identifier.url http://www.scopus.com/inward/record.url?partnerID=HzOxMe3b&scp=84906088054 -
dc.identifier.wosid 000338337700034 -
dc.language 영어 -
dc.publisher SPRINGER -
dc.title Representation of tropical subseasonal variability of precipitation in global reanalyses -
dc.type Article -
dc.description.isOpenAccess FALSE -
dc.relation.journalWebOfScienceCategory Meteorology & Atmospheric Sciences -
dc.relation.journalResearchArea Meteorology & Atmospheric Sciences -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -

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