Currents in Korea-Tsushima Strait during summer 1999
Results are presented from continuous current measurements across Korea‐Tsushima Strait between May and October 1999. The data are from eleven bottom‐mounted Acoustic Doppler Current Profilers that recorded full‐depth profiles of currents along two lines, one at each end of the Strait. The two secti...
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Veröffentlicht in: | Geophysical research letters 2000-10, Vol.27 (19), p.3033-3036 |
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creator | Perkins, H. Teague, W. J. Jacobs, G. A. Chang, K. I. Suk, M.-S. |
description | Results are presented from continuous current measurements across Korea‐Tsushima Strait between May and October 1999. The data are from eleven bottom‐mounted Acoustic Doppler Current Profilers that recorded full‐depth profiles of currents along two lines, one at each end of the Strait. The two sections show markedly different mean flow regimes. At the southern entrance, the cross‐section flow varies smoothly across the channel, showing a broad maximum at mid‐channel. The northern section is marked by strong spatial variability but in the mean consists of two streams, one on each side of the strait. Between the two is a regime of highly variable flow with a weak mean, presumably indicating the wake from Tsushima Island. Flow variability in time is described by statistical measures and by representative snapshots. |
doi_str_mv | 10.1029/2000GL011454 |
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Between the two is a regime of highly variable flow with a weak mean, presumably indicating the wake from Tsushima Island. Flow variability in time is described by statistical measures and by representative snapshots.</description><subject>Coastal oceanography, estuaries. Regional oceanography</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Marine</subject><subject>Physics of the oceans</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><recordid>eNqFkMtOwzAQRS0EEqWw4wOyQKwIjB-JM0uoaIqoQIIilpbjOhDIA-xE0L8nVSpgBauZxTl3NJeQQwqnFBieMQBI50CpiMQWGVEUIkwA5DYZAWC_Mxnvkj3vX3qQA6cjIiadc7ZufVDUwXXjrA4XvvPPRaWD-9bpog2WnSvqp8B3VWVdQBFxn-zkuvT2YDPH5GF6uZjMwvltejU5n4cmAsQQDY85SCYzIQUKnos4zwBiIRPOmKa41Jm2ImLRUnJuKUVmDEeWiCwSWcL4mBwPuW-uee-sb1VVeGPLUte26bxiNALKYvkvSBOIEZnowZMBNK7x3tlcvbn-VbdSFNS6Q_W7wx4_2uRqb3SZO12bwv84EcNErs-zAfsoSrv6M1Kld3PKY4m9FA5S4Vv7-S1p96r6j2SkHm9SBTNEkVxQNeVfvqyJ6g</recordid><startdate>20001001</startdate><enddate>20001001</enddate><creator>Perkins, H.</creator><creator>Teague, W. J.</creator><creator>Jacobs, G. 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Regional oceanography</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Marine</topic><topic>Physics of the oceans</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Perkins, H.</creatorcontrib><creatorcontrib>Teague, W. J.</creatorcontrib><creatorcontrib>Jacobs, G. A.</creatorcontrib><creatorcontrib>Chang, K. I.</creatorcontrib><creatorcontrib>Suk, M.-S.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</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>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Perkins, H.</au><au>Teague, W. J.</au><au>Jacobs, G. A.</au><au>Chang, K. I.</au><au>Suk, M.-S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Currents in Korea-Tsushima Strait during summer 1999</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2000-10-01</date><risdate>2000</risdate><volume>27</volume><issue>19</issue><spage>3033</spage><epage>3036</epage><pages>3033-3036</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>Results are presented from continuous current measurements across Korea‐Tsushima Strait between May and October 1999. The data are from eleven bottom‐mounted Acoustic Doppler Current Profilers that recorded full‐depth profiles of currents along two lines, one at each end of the Strait. The two sections show markedly different mean flow regimes. At the southern entrance, the cross‐section flow varies smoothly across the channel, showing a broad maximum at mid‐channel. The northern section is marked by strong spatial variability but in the mean consists of two streams, one on each side of the strait. Between the two is a regime of highly variable flow with a weak mean, presumably indicating the wake from Tsushima Island. Flow variability in time is described by statistical measures and by representative snapshots.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2000GL011454</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Coastal oceanography, estuaries. Regional oceanography Earth, ocean, space Exact sciences and technology External geophysics Marine Physics of the oceans |
title | Currents in Korea-Tsushima Strait during summer 1999 |
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