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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/mtc-m17@80/2007/07.16.11.57
Last Update2007:07.16.11.57.25 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m17@80/2007/07.16.11.57.27
Metadata Last Update2021:02.10.23.13.07 (UTC) administrator
Secondary KeyINPE-14988-PRE/9899
Citation KeyKouadioMachServ:2007:TrAtHu
TitleTropical Atlantic Hurricanes Originating from West Africa Mesoscale Convective Systems
FormatPapel; On-line.
Year2007
Access Date2024, Apr. 26
Secondary TypePRE CI
Number of Files1
Size532 KiB
2. Context
Author1 Kouadio, Y. K.
2 Machado, L. A. T.
3 Servain, J.
Group1
2 DSA-INPE-MCT-BR
Affiliation1 University of Cocody (Abidjan, Côte d’Ivoire)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Institut de Recherche pour le Développement (Paris, France)
Conference NameAGU Joint Assembly.
Conference LocationAcapulco - México
Date22 - 25 maio
Book TitleProceedings
Tertiary TypePoster Session
History (UTC)2007-11-27 12:47:22 :: estagiario -> administrator ::
2008-06-29 14:41:36 :: administrator -> estagiario ::
2010-05-11 17:00:20 :: estagiario -> administrator ::
2021-02-10 23:13:07 :: administrator -> marciana :: 2007
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
AbstractThis study focuses on the relationship between Mesoscale Convective Systems (MCSs) initiated in West Africa and subsequent cyclogenesis in North tropical Atlantic Ocean. MCS data are obtained from a convective cloud cluster tracking algorithm (FORTRACC) using Meteosat observations. We argue about a continuing propagation of fragmented stratiform parts of MCSs after their dissipations in the ocean. Ten occurrences during 2004-2005 of time lags and distances between MCS dissipations and hurricane initiations fairly agree with easterly wave propagations at a mean celerity of 9.7 m/s. It is shown that such a relationship occurs during a persisted SST anomaly dipole marked by a strong positive event in the Northern tropical Atlantic and a rather cold event in the Guinea Gulf.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > Tropical Atlantic Hurricanes...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
data URLhttp://urlib.net/ibi/sid.inpe.br/mtc-m17@80/2007/07.16.11.57
zipped data URLhttp://urlib.net/zip/sid.inpe.br/mtc-m17@80/2007/07.16.11.57
Languageen
Target Filewest_kouadio.pdf
User Groupadministrator
estagiario
Visibilityshown
Copy HolderSID/SCD
5. Allied materials
Next Higher Units8JMKD3MGPCW/43SRC6S
Citing Item Listsid.inpe.br/bibdigital/2021/01.03.02.10 1
Host Collectionlcp.inpe.br/ignes/2004/02.12.18.39
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
Empty Fieldsarchivingpolicy archivist callnumber copyright creatorhistory descriptionlevel dissemination documentstage doi e-mailaddress edition editor electronicmailaddress identifier isbn issn keywords label lineage mark mirrorrepository nextedition notes numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark type url versiontype volume
7. Description control
e-Mail (login)marciana
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