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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3LFCARB
Repositorysid.inpe.br/mtc-m21b/2016/04.07.16.54   (restricted access)
Last Update2016:07.04.17.45.04 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21b/2016/04.07.16.54.34
Metadata Last Update2018:06.04.02.40.39 (UTC) administrator
DOI10.1155/2016/2089418
ISSN1687-9309
Citation KeyMachadoJustPezz:2016:ImWiSt
TitleImpacts of wind stress changes on the global heat transport, baroclinic instability, and the thermohaline circulation
Year2016
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size3890 KiB
2. Context
Author1 Machado, Jeferson Prietsch
2 Justino, Flávio
3 Pezzi, Luciano Ponzi
Resume Identifier1
2
3 8JMKD3MGP5W/3C9JHM8
Group1
2
3 DSR-OBT-INPE-MCTI-GOV-BR
Affiliation1 Universidade Estadual Paulista (UNESP)
2 Universidade Federal de Viçosa (UFV)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1 jefpmac@gmail.com
2
3 luciano.pezzi@inpe.br
JournalAdvances in Meteorology
Volume2016
Pages2089418
Secondary MarkB4_GEOCIÊNCIAS B5_BIODIVERSIDADE
History (UTC)2016-04-07 16:54:34 :: simone -> administrator ::
2016-07-04 12:29:59 :: administrator -> simone :: 2016
2016-07-04 17:45:04 :: simone -> administrator :: 2016
2018-06-04 02:40:39 :: administrator -> simone :: 2016
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractThe wind stress is a measure of momentum transfer due to the relative motion between the atmosphere and the ocean. This study aims to investigate the anomalous pattern of atmospheric and oceanic circulations due to 50% increase in the wind stress over the equatorial region and the Southern Ocean. In this paper we use a coupled climate model of intermediate complexity (SPEEDO). The results show that the intensification of equatorial wind stress causes a decrease in sea surface temperature in the tropical region due to increased upwelling and evaporative cooling. On the other hand, the intensification of wind stress over the Southern Ocean induces a regional increase in the air and sea surface temperatures which in turn leads to a reduction in Antarctic sea ice thickness. This occurs in association with changes in the global thermohaline circulation strengthening the rate of Antarctic Bottom Water formation and a weakening of the North Atlantic Deep Water. Moreover, changes in the Southern Hemisphere thermal gradient lead to modified atmospheric and oceanic heat transports reducing the storm tracks and baroclinic activity.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Impacts of wind...
doc Directory Contentaccess
source Directory Contentthere are no files
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4. Conditions of access and use
Languageen
Target File1_machado_impacts.pdf
User Groupsimone
Reader Groupadministrator
simone
Visibilityshown
Archiving Policydenypublisher allowfinaldraft
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Mirror Repositoryurlib.net/www/2011/03.29.20.55
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.53.48 1
DisseminationWEBSCI; PORTALCAPES; SCOPUS.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn keywords label lineage mark month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
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