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Reference TypeJournal Article
Identifier8JMKD3MGP3W34P/3PUKG9E
Repositorysid.inpe.br/mtc-m21b/2017/11.08.12.47
Metadatasid.inpe.br/mtc-m21b/2017/11.08.12.47.37
Sitemtc-m21b.sid.inpe.br
DOI10.1357/002224017821836770
ISSN0022-2402
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Citation KeyMillerCGJMPPPST:2017:CoOcMo
Author 1 Miller, Arthur J.
 2 Collins, Mat
 3 Gualdi, Silvio
 4 Jensen, Tommy G.
 5 Misra, Vasu
 6 Pezzi, Luciano Ponzi
 7 Pierce, David W.
 8 Putrasahan, Dian
 9 Seo, Hyodae
10 Tseng, Yu-Heng
Resume Identifier 1
 2
 3
 4
 5
 6 8JMKD3MGP5W/3C9JHM8
Group 1
 2
 3
 4
 5
 6 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
Affiliation 1 Scripps Institution of Oceanography
 2 University of Exeter
 3 Centro Euro-Mediterraneo sui Cambiamenti Climatici
 4 U.S. Naval Research Laboratory
 5 Florida State University
 6 Instituto Nacional de Pesquisas Espaciais (INPE)
 7 Scripps Institution of Oceanography
 8 Max Planck Institute for Meteorology
 9 Woods Hole Oceanographic Institution
10 National Taiwan University
Author e-Mail Address 1 ajmiller@ucsd.edu
 2
 3
 4
 5
 6 luciano.pezzi@inpe.br
TitleCoupled ocean-atmosphere modeling and predictions
JournalJournal of Marine Research
Year2017
Volume75
Number3
MonthMay
KeywordsCLIMATE MODELING, CLIMATE PREDICTABILITY, DECADAL CLIMATE VARIABILITY, EL NIŅO SOUTHERN OSCILLATION, ENSO, GLOBAL WARMING, MONSOONS, OCEAN-ATMOSPHERELAND INTERACTIONS, REGIONAL CLIMATE DOWNSCALING.
AbstractKey aspects of the current state of the ability of global and regional climate models to represent dynamical processes and precipitation variations are summarized. Interannual, decadal, and global-warming timescales, wherein the influence of the oceans is relevant and the potential for predictability is highest, are emphasized. Oceanic influences on climate occur throughout the ocean and extend over land to affect many types of climate variations, including monsoons, the El Niņo Southern Oscillation, decadal oscillations, and the response to greenhouse gas emissions. The fundamental ideas of coupling between the ocean-atmosphere-land system are explained for these modes in both global and regional contexts. Global coupled climate models are needed to represent and understand the complicated processes involved and allow us to make predictions over land and sea. Regional coupled climate models are needed to enhance our interpretation of the fine-scale response. The mechanisms by which large-scale, low-frequency variations can influence shorter timescale variations and drive regionalscale effects are also discussed. In this light of these processes, the prospects for practical climate predictability are also presented.
Pages361-402
Languageen
Type of Workjournal article
Secondary TypePRE PI
DisseminationWEBSCI
AreaSRE
Secondary MarkB1_GEOCIĘNCIAS
Size13413 KiB
Number of Files1
Target Filemiller_coupled.pdf
Last Update2020:09.15.19.33.36 sid.inpe.br/mtc-m21b/2013/09.26.14.25.20 simone
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Content TypeExternal Contribution
Document Stagenot transferred
Version Typepublisher
Archiving Policyallowpublisher allowfinaldraft
Read Permissionallow from all
Next Higher Units8JMKD3MGPCW/3ER446E
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History2017-11-08 12:47:37 :: simone -> administrator ::
2017-11-08 12:47:38 :: administrator -> simone :: 2017
2017-11-08 12:49:02 :: simone -> administrator :: 2017
2018-06-04 02:27:58 :: administrator -> simone :: 2017
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