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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZQjxQKY/ScT9n
Repositorysid.inpe.br/ePrint@80/2007/11.19.18.53   (restricted access)
Last Update2007:11.19.17.53.23 (UTC) administrator
Metadata Repositorysid.inpe.br/ePrint@80/2007/11.19.18.53.26
Metadata Last Update2021:02.10.19.21.15 (UTC) administrator
Secondary KeyINPE-14960-PRE/9872
ISSN0177-7971
Citation KeyPrakkiSelu:2007:ChStUp
TitleCharacteristics and structure of an upper air cold vortex in the subtropics of South America
Year2007
Secondary Date200706
MonthJun.
Access Date2024, Apr. 27
Secondary TypePRE PI
Number of Files1
Size2275 KiB
2. Context
Author1 Prakki, Satyamurty
2 Seluchi, Marcelo Enrique
Group1 DMD-INPE-MCT-BR
2 DOP-INPE-MCT-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais,(INPE/CPTEC)
2 Instituto Nacional de Pesquisas Espaciais,(INPE/CPTEC)
e-Mail Addressdeicy@cptec.inpe.br
JournalMeteorology and Atmospheric Physics
Volume96
Number3-4
Pages203-220
ProgressePrint update
History (UTC)2011-04-28 19:09:41 :: deicy@cptec.inpe.br -> administrator ::
2021-02-10 19:21:15 :: administrator -> deicy@cptec.inpe.br :: 2007
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
KeywordsSouth America
potential vorticity
AbstractThe horizontal and vertical structures of an upper air cold core vortex over the subtropical latitudes of South America in the winter of 1999 reveal many features that are different from tropical upper tropospheric cold core vortices. The vortex in the present study is observed poleward of the subtropical jetstreak. In the middle troposphere, the center of the vortex is cooler than the periphery by 6 degrees C. The relative vorticity is greatest just below the tropopause and the vortex presents a slight eastward tilt in the vertical. The CPTEC Eta regional model simulation dataset has been used to study the life cycle of the vortex. Intensification and movement of the system are well simulated by the combined effect of divergence and vorticity advection at 500hPa. The Lifted Index and CAPE values at the mature stage of the system are not sufficiently high to explain the precipitation associated with the vortex. However, Q-vector analysis of the model simulation datasets support the observed precipitation. The precipitation pattern closely follows the 700hPa vertical velocity. These results indicate that the rain associated with the vortex has been forced by dynamical lifting rather than by thermodynamic processes. Upper tropospheric stable conditions are responsible for the shallowness of convection. The vortex presented here is different from subtropical cyclones, which develop over oceans and have higher intensities. The present vortex development somewhat resembles lee development.
AreaMET
Arrangement 1urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Characteristics and structure...
Arrangement 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDOP > Characteristics and structure...
doc Directory Contentaccess
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4. Conditions of access and use
Languageen
Target Fileprakki.pdf
User Groupadministrator
deicy@cptec.inpe.br
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Previous Editionsid.inpe.br/ePrint@80/2006/08.04.11.44
Next Higher Units8JMKD3MGPCW/43SKC35
8JMKD3MGPCW/43SQKNE
DisseminationWEBSCI; PORTALCAPES; COMPENDEX.
Host Collectionsid.inpe.br/mtc-m18@80/2008/03.17.15.17
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previouslowerunit project readergroup resumeid rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Description control
e-Mail (login)deicy@cptec.inpe.br
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