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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/449CTSL
Repositorysid.inpe.br/mtc-m21c/2021/03.02.18.30   (restricted access)
Last Update2021:03.02.18.30.41 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2021/03.02.18.30.41
Metadata Last Update2022:04.03.22.28.14 (UTC) administrator
DOI10.1007/s10546-020-00553-6
ISSN0006-8314
1573-1472
Citation KeyInnocentiniGonçCaetTess:2021:PaCO2
TitlePartitioning the CO 2 Flux Mediated by Droplets Released from Breaking Waves
Year2021
MonthJan.
Access Date2024, May 17
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size816 KiB
2. Context
Author1 Innocentini, Valdir
2 Gonçalves, Iury Angelo
3 Caetano, Ernesto
4 Tessarolo, Luciana de Freitas
Resume Identifier1 8JMKD3MGP5W/3C9JJB3
ORCID1
2 0000-0002-4367-5943
Group1 DIMNT-CGCT-INPE-MCTI-GOV-BR
2
3
4 DIMNT-CGCT-INPE-MCTI-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade Federal do Espírito Santo (UFES)
3 Universidade Nacional do Mexíco
4 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1 vinnocentini@hotmail.com
2 iury.goncalves@ufes.br
3 caetano@unam.mx
4 lutessarolo@hotmail.com
JournalBoundary-Layer Meteorology
Volume178
Number1
Pages21-41
Secondary MarkA1_ENGENHARIAS_I A2_MATEMÁTICA_/_PROBABILIDADE_E_ESTATÍSTICA A2_INTERDISCIPLINAR A2_GEOCIÊNCIAS A2_ENGENHARIAS_III B1_ENGENHARIAS_IV B1_CIÊNCIAS_AMBIENTAIS B3_ASTRONOMIA_/_FÍSICA
History (UTC)2021-03-02 18:30:41 :: simone -> administrator ::
2021-03-02 18:30:55 :: administrator -> simone :: 2021
2021-03-02 18:32:57 :: simone -> administrator :: 2021
2022-04-03 22:28:14 :: administrator -> simone :: 2021
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsAir–sea CO2 exchange · CO2 sea-droplet flux · Droplet–air gas gradient · Droplet lifetime · Droplet solubility
AbstractThe CO 2 flux from spume droplets occurs in two steps. First, the initial dropletair gas concentration gradient ∇ C is immediately removed with no change in the droplet solubility. Then, the solubility changes with droplet temperature T and radius r evolution, but the flux maintains the condition ∇ C= 0. The gas content of a droplet can be determined by ∇ C= 0 since the parameters T and r are known. Therefore, the net gas influx of a droplet depends on the values of T and r in its return to the sea. In the second step, the droplet temperature T evolves to an equilibrium temperature Teq, and the radius r is then reduced by evaporation at constant Teq. For the droplet spectrum, a cut-off radius rcut is used to separate short-lived (r> rcut, returning to the sea before T= Teq) and long-lived r≤ rcut conditions. The net influx is split into three contributions: the first (S2S) is mediated by short-lived mechanisms, and the second and the third by long-lived (S2L) mechanisms that are further separated into temperature-varying (S2LT) and radius-varying (S2LR) stages. The results show that, in the cases with large airsea temperature differences, the first stage S2S dominates the net gas input, but its importance decreases as the value of rcut increases. The temperature-varying stage S2LT is dominant in cases with both large values of rcut and large temperature differences, while the radius-varying stage S2LR increases as either the temperature difference decreases or as the value of rcut increases.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > Partitioning the CO...
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4. Conditions of access and use
Languageen
Target FileInnocentini2021_Article_PartitioningTheHboxCO2CO2FluxM.pdf
User Groupsimone
Reader Groupadministrator
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/46KUATE
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.15.01.22 3
sid.inpe.br/bibdigital/2022/04.03.22.23 1
DisseminationWEBSCI; PORTALCAPES; COMPENDEX.
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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