Wind and bathymetric forcing of the annual sea surface temperature signal in the East (Japan) Sea
The relationship between the annual cycle of sea surface temperature (SST) in the East (Japan) Sea and wind forcing and bathymetry is examined using AVHRR‐derived SST fields and satellite‐derived scatterometer wind fields. On the basin scale, SST north of the Subpolar Front (SPF) is characterized by...
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Veröffentlicht in: | Geophysical research letters 2005-03, Vol.32 (5), p.n/a |
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description | The relationship between the annual cycle of sea surface temperature (SST) in the East (Japan) Sea and wind forcing and bathymetry is examined using AVHRR‐derived SST fields and satellite‐derived scatterometer wind fields. On the basin scale, SST north of the Subpolar Front (SPF) is characterized by relatively larger amplitude (≥10°C) and variance (≥94%) and earlier phase than water to the south. Furthermore, north of the SPF, earlier SST cooling coincides with regions of high winds. On a much smaller spatial scale, the data show earlier SST cooling over the Siberian seamount is a result of the relatively shallow water over the seamount coupled with the complete erosion of the seasonal thermocline in mid February. |
doi_str_mv | 10.1029/2004GL022197 |
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On the basin scale, SST north of the Subpolar Front (SPF) is characterized by relatively larger amplitude (≥10°C) and variance (≥94%) and earlier phase than water to the south. Furthermore, north of the SPF, earlier SST cooling coincides with regions of high winds. 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Res. Lett</addtitle><description>The relationship between the annual cycle of sea surface temperature (SST) in the East (Japan) Sea and wind forcing and bathymetry is examined using AVHRR‐derived SST fields and satellite‐derived scatterometer wind fields. On the basin scale, SST north of the Subpolar Front (SPF) is characterized by relatively larger amplitude (≥10°C) and variance (≥94%) and earlier phase than water to the south. Furthermore, north of the SPF, earlier SST cooling coincides with regions of high winds. On a much smaller spatial scale, the data show earlier SST cooling over the Siberian seamount is a result of the relatively shallow water over the seamount coupled with the complete erosion of the seasonal thermocline in mid February.</description><subject>Marine</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNqFkU9v1DAQxa0KpC6lNz6ATxVIhI7_JI6PqGoX0KqVtoUerVln3Lpkk62dCPbbN8sixKk9jGak93szIz3G3gn4JEDaUwmg5wuQUlhzwGbCal3UAOYVmwHYaZamOmRvcn4AAAVKzBjexq7hONUKh_vtmoYUPQ998rG7433gwz1NcjdiyzMhz2MK6IkPtN5QwmFMxHO86yY5dn_gc8wDf_8NN9h94NeEb9nrgG2m47_9iH2_OL85-1IsruZfzz4vCl8KBUUjUHprGhFWXiBIL0NDQaOw1TRoKXQpVxWFRknVIGhhLWhfW4-ybKA06oid7PduUv84Uh7cOmZPbYsd9WN20oKFuoSXwbqyRijxIiiMklDK3emPe9CnPudEwW1SXGPaOgFul4z7P5kJl3v8V2xp-yzr5svFFGO1-7rYm2Ie6Pc_E6afrjLKlO72cu5-mLLWy2rpLtQTTuydJg</recordid><startdate>200503</startdate><enddate>200503</enddate><creator>Park, Kyung-Ae</creator><creator>Chung, Jong Yul</creator><creator>Kim, Kuh</creator><creator>Cornillon, Peter C.</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>7U5</scope><scope>8FD</scope><scope>L7M</scope><scope>H8D</scope></search><sort><creationdate>200503</creationdate><title>Wind and bathymetric forcing of the annual sea surface temperature signal in the East (Japan) Sea</title><author>Park, Kyung-Ae ; Chung, Jong Yul ; Kim, Kuh ; Cornillon, Peter C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5130-d1a2c97d1fbc1a02c2fdef4a196fde421452b6efd323da0419904c89ca25d0573</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Marine</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Park, Kyung-Ae</creatorcontrib><creatorcontrib>Chung, Jong Yul</creatorcontrib><creatorcontrib>Kim, Kuh</creatorcontrib><creatorcontrib>Cornillon, Peter C.</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Aerospace Database</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Park, Kyung-Ae</au><au>Chung, Jong Yul</au><au>Kim, Kuh</au><au>Cornillon, Peter C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Wind and bathymetric forcing of the annual sea surface temperature signal in the East (Japan) Sea</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2005-03</date><risdate>2005</risdate><volume>32</volume><issue>5</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>The relationship between the annual cycle of sea surface temperature (SST) in the East (Japan) Sea and wind forcing and bathymetry is examined using AVHRR‐derived SST fields and satellite‐derived scatterometer wind fields. On the basin scale, SST north of the Subpolar Front (SPF) is characterized by relatively larger amplitude (≥10°C) and variance (≥94%) and earlier phase than water to the south. Furthermore, north of the SPF, earlier SST cooling coincides with regions of high winds. On a much smaller spatial scale, the data show earlier SST cooling over the Siberian seamount is a result of the relatively shallow water over the seamount coupled with the complete erosion of the seasonal thermocline in mid February.</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2004GL022197</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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title | Wind and bathymetric forcing of the annual sea surface temperature signal in the East (Japan) Sea |
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