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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16d.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP7W/36GKUBP
Repositorysid.inpe.br/mtc-m19@80/2009/12.03.13.02   (restricted access)
Last Update2009:12.03.13.02.52 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m19@80/2009/12.03.13.02.54
Metadata Last Update2021:02.10.18.35.32 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.2151/jmsj.87A.381
ISSN0026-1165
Citation KeyInoueViRaHaWuMa:2009:LiCyDe
TitleLife cycle of deep convective systems over the Eastern Tropical Pacific observed by TRMM and GOES-W
Year2009
Access Date2024, Apr. 27
Secondary TypePRE PI
Number of Files1
Size1658 KiB
2. Context
Author1 Inoue, Toshiro
2 Vila, Daniel
3 Rajendran, Kavirajan
4 Hamada, Atsushi
5 Wu, Xiangqian
6 Machado, Luiz Augusto Toledo
Resume Identifier1
2
3
4
5
6 8JMKD3MGP5W/3C9JHMS
Group1
2
3
4
5
6 CPT-CPT-INPE-MCT-BR
Affiliation1 Center of Climate System Research, The University of Tokyo
2 Cooperative Institute for Climate Studies (CICS/ESSIC), University of Maryland at College Park
3 CSIR-Center for Mathematical Modeling and Computer Simulation, National Aerospace Laboraties
4 Graduate School of Science, Kyoto University
5 Center for Satellite Applications and Research/NOAA
6 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1
2
3
4
5
6 luiz.machado@cptec.inpe.br
e-Mail Addressdeicy.farabello@cptec.inpe.br
JournalJournal of the Meteorological Society of Japan
Volume87A
Pages381-391
Secondary MarkB1_GEOCIÊNCIAS A2_INTERDISCIPLINAR
History (UTC)2010-01-27 23:40:52 :: deicy -> banon ::
2010-01-27 23:51:38 :: banon -> administrator ::
2021-02-10 18:35:32 :: administrator -> marciana :: 2009
3. Content and structure
Is the master or a copy?is the master
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Transferable1
Content TypeExternal Contribution
Keywords**
AbstractThe life cycle of deep convective systems over the eastern tropical Pacific (30ºN to 30ºS, 180 to 90ºW) was studied in term of cloud types, as classified by a split window (11 um and 12 um). Hourly split window image data of Geostationary Operational Environmental Staellite (GOES-W) from January 2001 to December 2002 was used in this study. Deep convective systems consist mostly of optically thick cumulus type clouds in the earlier stage and a cirrus type cloud area that increases with time in the later stage. During this analysis period and over the analysis area, the life stage of deep convective system, to a large extent, can be identified by computing the percentage of cirrus type clouds within the deep convective system from a single snap shot of the split window image. Coincident Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (PR) observations were used to study the relationship between the percentage of cirrus type clouds within a deep convective system (i.e., its life stage) and the rainfall rate. It was found that the rainfall rate tends to be larger in the earlier stage of the life cycle when a smaller percentage of cirrus type cloud is present within the deep convection.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Life cycle of...
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4. Conditions of access and use
Languageen
Target File110007337738.pdf
User Groupadministrator
banon
deicy
Visibilityshown
Archiving Policydenypublisher denyfinaldraft
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Mirror Repositorysid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Next Higher Units8JMKD3MGPCW/3EUPEJL
DisseminationWEBSCI; PORTALCAPES.
Host Collectionsid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notes
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