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Future Amplification of Sea Surface Temperature Seasonality Due To Enhanced Ocean Stratification

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dc.contributor.authorAnila Rani Jo-
dc.contributor.authorJune-Yi Lee-
dc.contributor.authorAxel Timmermann-
dc.contributor.authorJin, Fei-Fei-
dc.contributor.authorRyohei Yamaguchi-
dc.contributor.authorGallego, Angeles-
dc.date.accessioned2022-07-28T04:43:34Z-
dc.date.available2022-07-28T04:43:34Z-
dc.date.created2022-06-02-
dc.date.issued2022-05-
dc.identifier.issn0094-8276-
dc.identifier.urihttps://pr.ibs.re.kr/handle/8788114/11941-
dc.description.abstract© 2022. The Authors.In many regions the projected future sea surface temperature (SST) response to greenhouse warming is larger in summer than in winter. What causes this amplification of the SST seasonal cycle has remained unclear. To determine robustness of the projected seasonal cycle intensification and ascertain underlying physical mechanisms we analyze a suite of historical and greenhouse warming simulations conducted with 13 coupled general circulation models in the Coupled Model Intercomparison Project Phase 5. In the Representative Concentration Pathway 8.5 scenario, the amplitude of SST seasonal cycle, defined as the difference between climatological maximum and minimum temperature, increases by 30% ± 20% on average by the end of 21st century. Analysis of a simplified mixed layer heat budget demonstrates that the amplification can be attributed to the increasing upper ocean stratification and hence shoaling of the annual-mean mixed layer. The projected intensification of SST seasonality may have important implications for future changes in marine ecosystems.-
dc.language영어-
dc.publisherJohn Wiley and Sons Inc-
dc.titleFuture Amplification of Sea Surface Temperature Seasonality Due To Enhanced Ocean Stratification-
dc.typeArticle-
dc.type.rimsART-
dc.identifier.wosid000796323100001-
dc.identifier.scopusid2-s2.0-85130093746-
dc.identifier.rimsid78240-
dc.contributor.affiliatedAuthorAnila Rani Jo-
dc.contributor.affiliatedAuthorJune-Yi Lee-
dc.contributor.affiliatedAuthorAxel Timmermann-
dc.contributor.affiliatedAuthorRyohei Yamaguchi-
dc.identifier.doi10.1029/2022GL098607-
dc.identifier.bibliographicCitationGeophysical Research Letters, v.49, no.9-
dc.relation.isPartOfGeophysical Research Letters-
dc.citation.titleGeophysical Research Letters-
dc.citation.volume49-
dc.citation.number9-
dc.type.docTypeArticle-
dc.description.journalClass1-
dc.description.journalClass1-
dc.description.isOpenAccessN-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.relation.journalResearchAreaGeology-
dc.relation.journalWebOfScienceCategoryGeosciences, Multidisciplinary-
dc.subject.keywordPlusSST ANNUAL CYCLE-
dc.subject.keywordPlusMIXED-LAYER-
dc.subject.keywordAuthorgreenhouse warming-
dc.subject.keywordAuthorheat budget analysis-
dc.subject.keywordAuthormixed layer depth-
dc.subject.keywordAuthorsea surface temperature-
dc.subject.keywordAuthorseasonal cycle amplification-
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Center for Climate Physics(기후물리 연구단) > 1. Journal Papers (저널논문)
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