Winter interactions between weather regimes and marine surface in the North Atlantic European region
This study aims at understanding the winter marine surface/atmosphere interactions in the North Atlantic European (NAE) region on intraseasonal timescales. The CNRMOM1d ocean model coupled with the GELATO3 sea ice model is forced with the ERA40 surface fluxes over the 1959–2001 period. Composites of...
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| Veröffentlicht in: | Geophysical research letters 2009-05, Vol.36 (9), p.np-n/a |
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| creator | Guemas, Virginie Salas-Mélia, David Kageyama, Masa Giordani, Hervé Voldoire, Aurore Sanchez-Gomez, Emilia |
| description | This study aims at understanding the winter marine surface/atmosphere interactions in the North Atlantic European (NAE) region on intraseasonal timescales. The CNRMOM1d ocean model coupled with the GELATO3 sea ice model is forced with the ERA40 surface fluxes over the 1959–2001 period. Composites of the simulated Sea Surface Temperature (SST) and sea ice concentration anomalies associated with each weather regime are computed. These are then prescribed to the ARPEGE Atmosphere General Circulation Model. We show that the interaction with the marine surface induces a negative feedback on the persistence of the NAO– regime, favours the transition from the Zonal regime toward the Atlantic Ridge regime and destabilizes the transition from the Blocking regime toward the Atlantic Ridge regime. |
| doi_str_mv | 10.1029/2009GL037551 |
| format | Article |
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We show that the interaction with the marine surface induces a negative feedback on the persistence of the NAO– regime, favours the transition from the Zonal regime toward the Atlantic Ridge regime and destabilizes the transition from the Blocking regime toward the Atlantic Ridge regime.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2009GL037551</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Atmosphere ; Atmospheres ; Atmospheric circulation ; Atmospheric sciences ; Climatology ; Cryosphere ; Earth Sciences ; Earth, ocean, space ; Exact sciences and technology ; General circulation models ; Ice ; Marine ; modeling ; Negative feedback ; Ocean, Atmosphere ; Ocean-atmosphere interaction ; Oceanography ; Oceans ; Ridges ; Sciences of the Universe ; Sea ice ; Sea surface temperature ; sea-ice/atmosphere interactions ; sub-monthly timescales ; Weather ; Winter</subject><ispartof>Geophysical research letters, 2009-05, Vol.36 (9), p.np-n/a</ispartof><rights>Copyright 2009 by the American Geophysical Union.</rights><rights>2009 INIST-CNRS</rights><rights>Copyright 2009 by American Geophysical Union</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4802-335777e85ff1f4c9567c897b95fdc51bae0f552122af268bd40b91fac7f5c8e63</citedby><cites>FETCH-LOGICAL-c4802-335777e85ff1f4c9567c897b95fdc51bae0f552122af268bd40b91fac7f5c8e63</cites><orcidid>0000-0003-0822-5880 ; 0000-0001-9585-7792 ; 0000-0001-5517-2473</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2009GL037551$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2009GL037551$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,776,780,881,1411,1427,11494,27903,27904,45553,45554,46387,46446,46811,46870</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=21562996$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://meteofrance.hal.science/meteo-00459493$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Guemas, Virginie</creatorcontrib><creatorcontrib>Salas-Mélia, David</creatorcontrib><creatorcontrib>Kageyama, Masa</creatorcontrib><creatorcontrib>Giordani, Hervé</creatorcontrib><creatorcontrib>Voldoire, Aurore</creatorcontrib><creatorcontrib>Sanchez-Gomez, Emilia</creatorcontrib><title>Winter interactions between weather regimes and marine surface in the North Atlantic European region</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>This study aims at understanding the winter marine surface/atmosphere interactions in the North Atlantic European (NAE) region on intraseasonal timescales. The CNRMOM1d ocean model coupled with the GELATO3 sea ice model is forced with the ERA40 surface fluxes over the 1959–2001 period. Composites of the simulated Sea Surface Temperature (SST) and sea ice concentration anomalies associated with each weather regime are computed. These are then prescribed to the ARPEGE Atmosphere General Circulation Model. We show that the interaction with the marine surface induces a negative feedback on the persistence of the NAO– regime, favours the transition from the Zonal regime toward the Atlantic Ridge regime and destabilizes the transition from the Blocking regime toward the Atlantic Ridge regime.</description><subject>Atmosphere</subject><subject>Atmospheres</subject><subject>Atmospheric circulation</subject><subject>Atmospheric sciences</subject><subject>Climatology</subject><subject>Cryosphere</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>General circulation models</subject><subject>Ice</subject><subject>Marine</subject><subject>modeling</subject><subject>Negative feedback</subject><subject>Ocean, Atmosphere</subject><subject>Ocean-atmosphere interaction</subject><subject>Oceanography</subject><subject>Oceans</subject><subject>Ridges</subject><subject>Sciences of the Universe</subject><subject>Sea 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interactions between weather regimes and marine surface in the North Atlantic European region</title><author>Guemas, Virginie ; Salas-Mélia, David ; Kageyama, Masa ; Giordani, Hervé ; Voldoire, Aurore ; Sanchez-Gomez, Emilia</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4802-335777e85ff1f4c9567c897b95fdc51bae0f552122af268bd40b91fac7f5c8e63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Atmosphere</topic><topic>Atmospheres</topic><topic>Atmospheric circulation</topic><topic>Atmospheric sciences</topic><topic>Climatology</topic><topic>Cryosphere</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>General circulation models</topic><topic>Ice</topic><topic>Marine</topic><topic>modeling</topic><topic>Negative feedback</topic><topic>Ocean, Atmosphere</topic><topic>Ocean-atmosphere 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Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Guemas, Virginie</au><au>Salas-Mélia, David</au><au>Kageyama, Masa</au><au>Giordani, Hervé</au><au>Voldoire, Aurore</au><au>Sanchez-Gomez, Emilia</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Winter interactions between weather regimes and marine surface in the North Atlantic European region</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2009-05</date><risdate>2009</risdate><volume>36</volume><issue>9</issue><spage>np</spage><epage>n/a</epage><pages>np-n/a</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>This study aims at understanding the winter marine surface/atmosphere interactions in the North Atlantic European (NAE) region on intraseasonal timescales. The CNRMOM1d ocean model coupled with the GELATO3 sea ice model is forced with the ERA40 surface fluxes over the 1959–2001 period. Composites of the simulated Sea Surface Temperature (SST) and sea ice concentration anomalies associated with each weather regime are computed. These are then prescribed to the ARPEGE Atmosphere General Circulation Model. We show that the interaction with the marine surface induces a negative feedback on the persistence of the NAO– regime, favours the transition from the Zonal regime toward the Atlantic Ridge regime and destabilizes the transition from the Blocking regime toward the Atlantic Ridge regime.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2009GL037551</doi><tpages>6</tpages><orcidid>https://orcid.org/0000-0003-0822-5880</orcidid><orcidid>https://orcid.org/0000-0001-9585-7792</orcidid><orcidid>https://orcid.org/0000-0001-5517-2473</orcidid><oa>free_for_read</oa></addata></record> |
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| ispartof | Geophysical research letters, 2009-05, Vol.36 (9), p.np-n/a |
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| language | eng |
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| source | Wiley Free Content; Wiley-Blackwell AGU Digital Library; Wiley Online Library Journals Frontfile Complete; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Atmosphere Atmospheres Atmospheric circulation Atmospheric sciences Climatology Cryosphere Earth Sciences Earth, ocean, space Exact sciences and technology General circulation models Ice Marine modeling Negative feedback Ocean, Atmosphere Ocean-atmosphere interaction Oceanography Oceans Ridges Sciences of the Universe Sea ice Sea surface temperature sea-ice/atmosphere interactions sub-monthly timescales Weather Winter |
| title | Winter interactions between weather regimes and marine surface in the North Atlantic European region |
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