Publicação
Differences in coastal and oceanic SST trends north of Yucatan Peninsula
| Resumo: | The coastal area north of Yucatan has experienced a cooling SST trend from 1982 to 2015 during the upwelling season (May–September) that contrasts with the warming observed at the adjacent ocean area. Different drivers were analyzed to identify the possible causes of that unusual coastal cooling. Changes in coastal upwelling and in sea-atmosphere heat fluxes are not consistent with the observed coastal cooling. The eastward shift of the Yucatan Current observed over the last decades is hypothesized as the most probable cause of coastal cooling. This shift enhances the vertical transport of cold deeper water to the continental shelf from where it is pumped to the surface by upwelling favorable westerly winds. |
|---|---|
| Autores principais: | Varela, R. |
| Outros Autores: | Costoya, X.; Enriquez, C.; Santos, F.; Gómez-Gesteira, M. |
| Assunto: | Upwelling Yucatan Sea surface temperature Wind Current direction Shelf dynamics Warming Cooling |
| Ano: | 2018 |
| País: | Portugal |
| Tipo de documento: | artigo |
| Tipo de acesso: | acesso aberto |
| Instituição associada: | Universidade de Aveiro |
| Idioma: | inglês |
| Origem: | RIA - Repositório Institucional da Universidade de Aveiro |
| _version_ | 1877769278366679040 |
|---|---|
| author | Varela, R. |
| author2 | Costoya, X. Enriquez, C. Santos, F. Gómez-Gesteira, M. |
| author2_role | author author author author |
| author_facet | Varela, R. Costoya, X. Enriquez, C. Santos, F. Gómez-Gesteira, M. |
| author_role | author |
| country_str | PT |
| creators_json_txt | [{\"Person.name\":\"Varela, R.\"},{\"Person.name\":\"Costoya, X.\"},{\"Person.name\":\"Enriquez, C.\"},{\"Person.name\":\"Santos, F.\"},{\"Person.name\":\"Gómez-Gesteira, M.\"}] |
| datacite.creators.creator.creatorName.fl_str_mv | Varela, R. Costoya, X. Enriquez, C. Santos, F. Gómez-Gesteira, M. |
| datacite.date.Accepted.fl_str_mv | 2018-06-01T00:00:00Z |
| datacite.date.available.fl_str_mv | 2023-04-14T10:02:32Z |
| datacite.date.embargoed.fl_str_mv | 2023-04-14T10:02:32Z |
| datacite.rights.fl_str_mv | http://purl.org/coar/access_right/c_abf2 |
| datacite.subjects.subject.fl_str_mv | Upwelling Yucatan Sea surface temperature Wind Current direction Shelf dynamics Warming Cooling |
| datacite.titles.title.fl_str_mv | Differences in coastal and oceanic SST trends north of Yucatan Peninsula |
| dc.creator.none.fl_str_mv | Varela, R. Costoya, X. Enriquez, C. Santos, F. Gómez-Gesteira, M. |
| dc.date.Accepted.fl_str_mv | 2018-06-01T00:00:00Z |
| dc.date.available.fl_str_mv | 2023-04-14T10:02:32Z |
| dc.date.embargoed.fl_str_mv | 2023-04-14T10:02:32Z |
| dc.format.none.fl_str_mv | application/pdf |
| dc.identifier.none.fl_str_mv | http://hdl.handle.net/10773/37029 |
| dc.language.none.fl_str_mv | eng |
| dc.publisher.none.fl_str_mv | Elsevier |
| dc.rights.none.fl_str_mv | http://purl.org/coar/access_right/c_abf2 |
| dc.subject.none.fl_str_mv | Upwelling Yucatan Sea surface temperature Wind Current direction Shelf dynamics Warming Cooling |
| dc.title.fl_str_mv | Differences in coastal and oceanic SST trends north of Yucatan Peninsula |
| dc.type.none.fl_str_mv | http://purl.org/coar/resource_type/c_6501 |
| description | The coastal area north of Yucatan has experienced a cooling SST trend from 1982 to 2015 during the upwelling season (May–September) that contrasts with the warming observed at the adjacent ocean area. Different drivers were analyzed to identify the possible causes of that unusual coastal cooling. Changes in coastal upwelling and in sea-atmosphere heat fluxes are not consistent with the observed coastal cooling. The eastward shift of the Yucatan Current observed over the last decades is hypothesized as the most probable cause of coastal cooling. This shift enhances the vertical transport of cold deeper water to the continental shelf from where it is pumped to the surface by upwelling favorable westerly winds. |
| dirty | 0 |
| eu_rights_str_mv | openAccess |
| format | article |
| id | ria_bad3353cdc9d42c0f5c86e7f479d5be6 |
| identifier.url.fl_str_mv | http://hdl.handle.net/10773/37029 |
| inst_facet_str | urn:organizationAcronym:ua{{{_:::_}}}Universidade de Aveiro |
| instacron_str | ua |
| institution | Universidade de Aveiro |
| instname_str | Universidade de Aveiro |
| language | eng |
| network_acronym_str | ria |
| network_name_str | RIA - Repositório Institucional da Universidade de Aveiro |
| oai_identifier_str | oai:ria.ua.pt:10773/37029 |
| organization_str_mv | urn:organizationAcronym:ua |
| person_str_mv | Varela, R. Costoya, X. Enriquez, C. Santos, F. Gómez-Gesteira, M. |
| publishDate | 2018 |
| publisher.none.fl_str_mv | Elsevier |
| repo_facet_str | urn:repositoryAcronym:ria{{{_:::_}}}RIA - Repositório Institucional da Universidade de Aveiro |
| reponame_str | RIA - Repositório Institucional da Universidade de Aveiro |
| repository_id_str | urn:repositoryAcronym:ria |
| service_str_mv | urn:repositoryAcronym:ria |
| spelling | pt_PTThe coastal area north of Yucatan has experienced a cooling SST trend from 1982 to 2015 during the upwelling season (May–September) that contrasts with the warming observed at the adjacent ocean area. Different drivers were analyzed to identify the possible causes of that unusual coastal cooling. Changes in coastal upwelling and in sea-atmosphere heat fluxes are not consistent with the observed coastal cooling. The eastward shift of the Yucatan Current observed over the last decades is hypothesized as the most probable cause of coastal cooling. This shift enhances the vertical transport of cold deeper water to the continental shelf from where it is pumped to the surface by upwelling favorable westerly winds.application/pdfengElsevierpt_PTDifferences in coastal and oceanic SST trends north of Yucatan PeninsulaVarela, R.Costoya, X.Enriquez, C.Santos, F.Gómez-Gesteira, M.Handlehttp://hdl.handle.net/10773/37029ISSNIsPartOf0924-7963DOIIsPartOf10.1016/j.jmarsys.2018.03.0062023-04-14T10:02:32Z2018-06-01T00:00:00Z2018-06http://purl.org/coar/access_right/c_abf2open accesspt_PTUpwellingpt_PTYucatanpt_PTSea surface temperaturept_PTWindpt_PTCurrent directionpt_PTShelf dynamicspt_PTWarmingpt_PTCooling2208723 byteshttp://purl.org/coar/access_right/c_abf2application/pdffulltexthttps://ria.ua.pt/bitstream/10773/37029/1/Differences%20in%20coastal%20and%20oceanic%20SST%20trends%20north%20of%20Yucatan.pdfliteraturehttp://purl.org/coar/resource_type/c_6501journal article |
| spellingShingle | Differences in coastal and oceanic SST trends north of Yucatan Peninsula Varela, R. Upwelling Yucatan Sea surface temperature Wind Current direction Shelf dynamics Warming Cooling |
| status | SINGLETON |
| subject.fl_str_mv | Upwelling Yucatan Sea surface temperature Wind Current direction Shelf dynamics Warming Cooling |
| title | Differences in coastal and oceanic SST trends north of Yucatan Peninsula |
| title_full | Differences in coastal and oceanic SST trends north of Yucatan Peninsula |
| title_fullStr | Differences in coastal and oceanic SST trends north of Yucatan Peninsula |
| title_full_unstemmed | Differences in coastal and oceanic SST trends north of Yucatan Peninsula |
| title_short | Differences in coastal and oceanic SST trends north of Yucatan Peninsula |
| title_sort | Differences in coastal and oceanic SST trends north of Yucatan Peninsula |
| topic | Upwelling Yucatan Sea surface temperature Wind Current direction Shelf dynamics Warming Cooling |
| topic_facet | Upwelling Yucatan Sea surface temperature Wind Current direction Shelf dynamics Warming Cooling |
| url | http://hdl.handle.net/10773/37029 |
| visible | 1 |
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