Relationship between satellite-observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan)
The relationship between cold surface water along the Primorye coast and sea ice in the Tatar Strait of the northern East Sea (the Sea of Japan) is examined by analyzing sea surface temperatures (SST) from NOAA/AVHRR, sea ice concentrations from SSM/I, wind vectors from QuikSCAT, and position data f...
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Veröffentlicht in: | Geophysical research letters 2006-05, Vol.33 (10), p.n.-n/a |
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creator | Park, Kyung-Ae Kim, Kuh Cornillon, Peter C. Chung, Jong Yul |
description | The relationship between cold surface water along the Primorye coast and sea ice in the Tatar Strait of the northern East Sea (the Sea of Japan) is examined by analyzing sea surface temperatures (SST) from NOAA/AVHRR, sea ice concentrations from SSM/I, wind vectors from QuikSCAT, and position data from satellite‐tracked drifting buoys. Relatively low SSTs along the Primorye coast in spring and early summer are attributed to sea ice melted water advected to the southwest as the Liman Cold Current (LCC). Monthly to year‐to‐year variations of SSTs along the Primorye coast in spring and early summer are negatively correlated with those of the sea ice concentration in the Tatar Strait during the previous winter. Translational speeds from the surface drifter and SST anomalies demonstrate that the LCC significantly varies by 2–18 km/day both in space and time. |
doi_str_mv | 10.1029/2005GL025611 |
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Relatively low SSTs along the Primorye coast in spring and early summer are attributed to sea ice melted water advected to the southwest as the Liman Cold Current (LCC). Monthly to year‐to‐year variations of SSTs along the Primorye coast in spring and early summer are negatively correlated with those of the sea ice concentration in the Tatar Strait during the previous winter. Translational speeds from the surface drifter and SST anomalies demonstrate that the LCC significantly varies by 2–18 km/day both in space and time.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2005GL025611</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Marine</subject><ispartof>Geophysical research letters, 2006-05, Vol.33 (10), p.n.-n/a</ispartof><rights>Copyright 2006 by the American Geophysical Union.</rights><rights>2006 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5432-7b5a7114aa1d6c3600d91ac6e43642f3a46679a4aca04b59b33c61c143d7ad03</citedby><cites>FETCH-LOGICAL-c5432-7b5a7114aa1d6c3600d91ac6e43642f3a46679a4aca04b59b33c61c143d7ad03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2005GL025611$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2005GL025611$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=17893772$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Park, Kyung-Ae</creatorcontrib><creatorcontrib>Kim, Kuh</creatorcontrib><creatorcontrib>Cornillon, Peter C.</creatorcontrib><creatorcontrib>Chung, Jong Yul</creatorcontrib><title>Relationship between satellite-observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan)</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>The relationship between cold surface water along the Primorye coast and sea ice in the Tatar Strait of the northern East Sea (the Sea of Japan) is examined by analyzing sea surface temperatures (SST) from NOAA/AVHRR, sea ice concentrations from SSM/I, wind vectors from QuikSCAT, and position data from satellite‐tracked drifting buoys. Relatively low SSTs along the Primorye coast in spring and early summer are attributed to sea ice melted water advected to the southwest as the Liman Cold Current (LCC). Monthly to year‐to‐year variations of SSTs along the Primorye coast in spring and early summer are negatively correlated with those of the sea ice concentration in the Tatar Strait during the previous winter. Translational speeds from the surface drifter and SST anomalies demonstrate that the LCC significantly varies by 2–18 km/day both in space and time.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Marine</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqFkU9v1DAQxSNEJZaWGx_AFxBIDYz_xI6PqCopVQRVqeBoTZwJNaTJYqdsl0_fpFsBJ3ry-Pk3b2y_LHvO4Q0HYd8KgKKqQRSa80fZilul8hLAPM5WAHauhdFPsqcpfQcACZKvst_n1OMUxiFdhjVraNoQDSzhRH0fJsrHJlH8RS3zY9-yzaxHhv04fGPTJbGzGK7GuKX5FNPEcGhZImTBEwvDHXG86J9n7dWyW4qxY6e4xuH1QbbXYZ_o2f26n128P744OsnrT9WHo3d17gslRW6aAg3nCpG32ksN0FqOXpOSWolOotLaWFToEVRT2EZKr7nnSrYGW5D72cud7TqOP68pTe4qJD8_Dwcar5MTFgSU0j4MlmA1SPEgyA0v-RzBDB7uQB_HlCJ1bj1_GMat4-CWxNy_ic34i3tfTB77LuLgQ_rbY0orjVnmix23CT1t_-vpqvNacHF36XzXFNJEN3-aMP5w2khTuK8fK2e-1PaMQ-VO5S0vhrG5</recordid><startdate>200605</startdate><enddate>200605</enddate><creator>Park, Kyung-Ae</creator><creator>Kim, Kuh</creator><creator>Cornillon, Peter C.</creator><creator>Chung, Jong Yul</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</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>8FD</scope><scope>FR3</scope><scope>KR7</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>200605</creationdate><title>Relationship between satellite-observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan)</title><author>Park, Kyung-Ae ; Kim, Kuh ; Cornillon, Peter C. ; Chung, Jong Yul</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5432-7b5a7114aa1d6c3600d91ac6e43642f3a46679a4aca04b59b33c61c143d7ad03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Marine</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Park, Kyung-Ae</creatorcontrib><creatorcontrib>Kim, Kuh</creatorcontrib><creatorcontrib>Cornillon, Peter C.</creatorcontrib><creatorcontrib>Chung, Jong Yul</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</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>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Park, Kyung-Ae</au><au>Kim, Kuh</au><au>Cornillon, Peter C.</au><au>Chung, Jong Yul</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Relationship between satellite-observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan)</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2006-05</date><risdate>2006</risdate><volume>33</volume><issue>10</issue><spage>n.</spage><epage>n/a</epage><pages>n.-n/a</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The relationship between cold surface water along the Primorye coast and sea ice in the Tatar Strait of the northern East Sea (the Sea of Japan) is examined by analyzing sea surface temperatures (SST) from NOAA/AVHRR, sea ice concentrations from SSM/I, wind vectors from QuikSCAT, and position data from satellite‐tracked drifting buoys. Relatively low SSTs along the Primorye coast in spring and early summer are attributed to sea ice melted water advected to the southwest as the Liman Cold Current (LCC). Monthly to year‐to‐year variations of SSTs along the Primorye coast in spring and early summer are negatively correlated with those of the sea ice concentration in the Tatar Strait during the previous winter. Translational speeds from the surface drifter and SST anomalies demonstrate that the LCC significantly varies by 2–18 km/day both in space and time.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2005GL025611</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Earth sciences Earth, ocean, space Exact sciences and technology Marine |
title | Relationship between satellite-observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan) |
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