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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/44Q786B
Repositorysid.inpe.br/mtc-m21c/2021/06.01.17.30   (restricted access)
Last Update2021:06.01.17.30.26 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2021/06.01.17.30.26
Metadata Last Update2022:04.03.22.39.39 (UTC) administrator
DOI10.1038/s41598-021-89985-9
ISSN2045-2322
Citation KeyPezziSSMCPQRJSCBVAMR:2021:OcEdMo
TitleOceanic eddy-induced modifications to air–sea heat and CO2 fluxes in the Brazil-Malvinas Confluence
Year2021
MonthDec.
Access Date2024, May 19
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size2996 KiB
2. Context
Author 1 Pezzi, Luciano Ponzi
 2 Souza, Ronald Buss de
 3 Santini, Marcelo Freitas
 4 Miller, Aarthur J.
 5 Carvalho, Jonas Takeo
 6 Parise, Cláudia K.
 7 Quadro, Mário F.
 8 Rosa, Eliana Bertol
 9 Justino, Flávio
10 Sutil, Ueslei Adriano
11 Cabrera, Mylene Jaen
12 Babanin, Alexander V.
13 Voermans, Joey
14 Nascimento
15 Ernani
16 L.
17 Alves, Rita de Cássia Marques
18 Munchow, Gabriel B.
19 Rubert, Joel
Resume Identifier 1 8JMKD3MGP5W/3C9JHM8
 2 8JMKD3MGP5W/3C9JJ6U
Group 1 DIOTG-CGCT-INPE-MCTI-GOV-BR
 2 DIMNT-CGCT-INPE-MCTI-GOV-BR
 3 DIOTG-CGCT-INPE-MCTI-GOV-BR
 4
 5 DIOTG-CGCT-INPE-MCTI-GOV-BR
 6
 7
 8 DIOTG-CGCT-INPE-MCTI-GOV-BR
 9
10 DIOTG-CGCT-INPE-MCTI-GOV-BR
11 CGCT-CGCT-INPE-MCTI-GOV-BR
12
13
14
15
16
17 COESU-CGGO-INPE-MCTI-GOV-BR
Affiliation 1 Instituto Nacional de Pesquisas Espaciais (INPE)
 2 Instituto Nacional de Pesquisas Espaciais (INPE)
 3 Instituto Nacional de Pesquisas Espaciais (INPE)
 4 University of California
 5 Instituto Nacional de Pesquisas Espaciais (INPE)
 6 Universidade Federal do Maranhão (UFMA)
 7 Instituto Federal de Santa Catarina (IFSC)
 8 Instituto Nacional de Pesquisas Espaciais (INPE)
 9 Universidade Federal de Viçosa (UFV)
10 Instituto Nacional de Pesquisas Espaciais (INPE)
11 Instituto Nacional de Pesquisas Espaciais (INPE)
12 University of Melbourne
13 University of Melbourne
14 Universidade Federal de Santa Maria (UFSM)
15 Universidade Federal do Rio Grande do Sul (UFRGS)
16 Universidade Federal do Rio Grande do Sul (UFRGS)
17 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address 1 luciano.pezzi@inpe.br
 2 ronaldbuss@hotmail.com
 3
 4
 5 jtcarvalho@gmail.com
 6
 7
 8 elianaocn@gmail.com
 9
10 uesleisutil1@gmail.com
11 mylecabrera90@gmail.com
JournalScientific Reports
Volume11
Number1
Pagese10648
Secondary MarkB2_BIODIVERSIDADE B3_ODONTOLOGIA B3_LETRAS_/_LINGUÍSTICA C_CIÊNCIAS_BIOLÓGICAS_III C_BIOTECNOLOGIA C_ASTRONOMIA_/_FÍSICA
History (UTC)2021-06-01 17:37:39 :: simone -> administrator :: 2021
2021-06-22 19:11:19 :: administrator -> simone :: 2021
2021-06-22 21:04:36 :: simone -> administrator :: 2021
2022-04-03 22:39:39 :: administrator -> simone :: 2021
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractSea surface temperature (SST) anomalies caused by a warm core eddy (WCE) in the Southwestern Atlantic Ocean (SWA) rendered a crucial influence on modifying the marine atmospheric boundary layer (MABL). During the first cruise to support the Antarctic Modeling and Observation System (ATMOS) project, a WCE that was shed from the Brazil Current was sampled. Apart from traditional meteorological measurements, we used the Eddy Covariance method to directly measure the oceanatmosphere sensible heat, latent heat, momentum, and carbon dioxide (CO2) fluxes. The mechanisms of pressure adjustment and vertical mixing that can make the MABL unstable were both identified. The WCE also acted to increase the surface winds and heat fluxes from the ocean to the atmosphere. Oceanic regions at middle and high latitudes are expected to absorb atmospheric CO2, and are thereby considered as sinks, due to their cold waters. Instead, the presence of this WCE in midlatitudes, surrounded by predominantly cold waters, caused the ocean to locally act as a CO2 source. The contribution to the atmosphere was estimated as 0.3 ± 0.04 mmol m−2 day−1, averaged over the sampling period. The CO2 transfer velocity coefficient (K) was determined using a quadratic fit and showed an adequate representation of oceanatmosphere fluxes. The oceanatmosphere CO2, momentum, and heat fluxes were each closely correlated with the SST. The increase of SST inside the WCE clearly resulted in larger magnitudes of all of the oceanatmosphere fluxes studied here. This study adds to our understanding of how oceanic mesoscale structures, such as this WCE, affect the overlying atmosphere.
AreaSRE
Arrangement 1urlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > Oceanic eddy-induced modifications...
Arrangement 2urlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGGO > Oceanic eddy-induced modifications...
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4. Conditions of access and use
Languageen
Target Files41598-021-89985-9.pdf
User Groupsimone
Reader Groupadministrator
simone
Visibilityshown
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/46KUATE
8JMKD3MGPCW/46KUBT5
Citing Item Listsid.inpe.br/bibdigital/2022/04.03.22.35 11
sid.inpe.br/bibdigital/2022/04.03.22.23 3
sid.inpe.br/mtc-m21/2012/07.13.14.53.48 2
DisseminationWEBSCI; PORTALCAPES; SCOPUS.
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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