Loading…
STUDY OF WATER—TRANSPORT THROUGH SOME MAIN STRAITS IN THE EAST CHINA SEA AND SOUTH CHINA SEA
OCCAM global ocean model results were applied to calculate the monthly water transport through 7 straits around the East China Sea(ECS)and the South china Sea(SCS).Analysis of the features of velocity profiles and their variations in the Togara Strait,Luzon Strait and Eastern Taiwan Strait showed th...
Saved in:
Published in: | Chinese journal of oceanology and limnology 2002-12, Vol.20 (4), p.293-302 |
---|---|
Main Author: | |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-c2221-7fd5b3f19301328c9969dff4b1421eaccce83749e982c2bac1190e3737a37f0e3 |
---|---|
cites | cdi_FETCH-LOGICAL-c2221-7fd5b3f19301328c9969dff4b1421eaccce83749e982c2bac1190e3737a37f0e3 |
container_end_page | 302 |
container_issue | 4 |
container_start_page | 293 |
container_title | Chinese journal of oceanology and limnology |
container_volume | 20 |
creator | 鲍献文 高郭平 吴德星 |
description | OCCAM global ocean model results were applied to calculate the monthly water transport through 7 straits around the East China Sea(ECS)and the South china Sea(SCS).Analysis of the features of velocity profiles and their variations in the Togara Strait,Luzon Strait and Eastern Taiwan Strait showed that;1)the velocity profiles had striped pattern in the Eastern Taiwan Strait,where monthly flux varied from 22.4 to 28.1 Sv and annual mean was about 25.8 Sv;2)the profiles of velocity in the Togara Strait were characterized by core structure,and monthly flux varied from 23.3 to 31.4 Sv,with annual mean of about 27.9 Sv;3)water flowed from the SCS to the ECS in the Taiwan Strait,with maximum flux of 3.1 Sv in July and minimum of 0.9 Sv in November;4)the flux in the Tsushima Strait varied by only about 0.4 Sv by season and its annual mean was about 2.3 Sv;5)Kuroshio water flowed into the SCS in the Luzon Strait throughout the year and the velocity profiles were characterized by multi-core structure.The flux in the Luzon Strait was minimun in June(about 2.4 Sv)and maximum in February(about 9.0 Sv),and its annual mean was 4.8 Sv;6)the monthly flux in the Mindoro Strait was maximum in December(3.0 Sv)and minimum in June(Only 0.1 Sv),and its annual mean was 1.3 Sv;7)Karimata Strait water flowed into the SCS from May to August,with maximum in-flow flux of about 0.75 Sv in June and flowed out from September to April at maximum outflow flux of 3.9 Sv in January.The annual mean flux was about 1.35 Sv. |
doi_str_mv | 10.1007/BF02847918 |
format | article |
fullrecord | <record><control><sourceid>wanfang_jour_proqu</sourceid><recordid>TN_cdi_wanfang_journals_zghyhzxb200204001</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>7616658</cqvip_id><wanfj_id>zghyhzxb200204001</wanfj_id><sourcerecordid>zghyhzxb200204001</sourcerecordid><originalsourceid>FETCH-LOGICAL-c2221-7fd5b3f19301328c9969dff4b1421eaccce83749e982c2bac1190e3737a37f0e3</originalsourceid><addsrcrecordid>eNp10d1KwzAUB_AgCs7pjU8QFQSF6knSNs1lnZ0d6Cprhnhj6GKyTWerrcOPKx_CJ_RJjEwUBK9ySH78DycHoU0CBwSAHx51gUY-FyRaQi0iBPMCgGAZtYAGvudDIFbRWtPcADDhg2ihq1wOjy9x1sUXsUwGH2_vchD38_NsILFMB9nwJMV5dpbgs7jXx7l77Mkcu1KmCU7iXOJO2uvHOE9iHPePnR3K9PduHa3YYtaYje-zjYbdRHZS7zQ76XXiU09TSonH7XUwYpYIBoTRSAsRimtr_RHxKTGF1tpEjPvCiIhqOio0IQIM44wXjFtXtdHeIvepKG1RjtVNNa9L11G9jicvk9fnEQWg4IPLb6Pdhb2vq4e5aR7V3bTRZjYrSlPNG0Ui91ksCB3c-QN_UqkgXIRRKLhT2_8qCFwUYV899xdI11XT1Maq-3p6V9QvioD62pz63ZzDW994UpXjh6kbx418a6czo3hIwjCI2CfVEYut</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>205025131</pqid></control><display><type>article</type><title>STUDY OF WATER—TRANSPORT THROUGH SOME MAIN STRAITS IN THE EAST CHINA SEA AND SOUTH CHINA SEA</title><source>Springer Link</source><creator>鲍献文 高郭平 吴德星</creator><creatorcontrib>鲍献文 高郭平 吴德星</creatorcontrib><description>OCCAM global ocean model results were applied to calculate the monthly water transport through 7 straits around the East China Sea(ECS)and the South china Sea(SCS).Analysis of the features of velocity profiles and their variations in the Togara Strait,Luzon Strait and Eastern Taiwan Strait showed that;1)the velocity profiles had striped pattern in the Eastern Taiwan Strait,where monthly flux varied from 22.4 to 28.1 Sv and annual mean was about 25.8 Sv;2)the profiles of velocity in the Togara Strait were characterized by core structure,and monthly flux varied from 23.3 to 31.4 Sv,with annual mean of about 27.9 Sv;3)water flowed from the SCS to the ECS in the Taiwan Strait,with maximum flux of 3.1 Sv in July and minimum of 0.9 Sv in November;4)the flux in the Tsushima Strait varied by only about 0.4 Sv by season and its annual mean was about 2.3 Sv;5)Kuroshio water flowed into the SCS in the Luzon Strait throughout the year and the velocity profiles were characterized by multi-core structure.The flux in the Luzon Strait was minimun in June(about 2.4 Sv)and maximum in February(about 9.0 Sv),and its annual mean was 4.8 Sv;6)the monthly flux in the Mindoro Strait was maximum in December(3.0 Sv)and minimum in June(Only 0.1 Sv),and its annual mean was 1.3 Sv;7)Karimata Strait water flowed into the SCS from May to August,with maximum in-flow flux of about 0.75 Sv in June and flowed out from September to April at maximum outflow flux of 3.9 Sv in January.The annual mean flux was about 1.35 Sv.</description><identifier>ISSN: 0254-4059</identifier><identifier>ISSN: 2096-5508</identifier><identifier>EISSN: 1993-5005</identifier><identifier>EISSN: 2523-3521</identifier><identifier>DOI: 10.1007/BF02847918</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Annual ; Fluctuations ; Inflow ; Marine ; Monthly ; Ocean circulation ; Ocean models ; Oceanography ; Outflow ; Straits ; Studies ; Velocity ; Velocity distribution ; Velocity profiles ; Water ; Water transport ; Waterways</subject><ispartof>Chinese journal of oceanology and limnology, 2002-12, Vol.20 (4), p.293-302</ispartof><rights>Science Press 2002</rights><rights>Science Press 2002.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2221-7fd5b3f19301328c9969dff4b1421eaccce83749e982c2bac1190e3737a37f0e3</citedby><cites>FETCH-LOGICAL-c2221-7fd5b3f19301328c9969dff4b1421eaccce83749e982c2bac1190e3737a37f0e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/84119X/84119X.jpg</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids></links><search><creatorcontrib>鲍献文 高郭平 吴德星</creatorcontrib><title>STUDY OF WATER—TRANSPORT THROUGH SOME MAIN STRAITS IN THE EAST CHINA SEA AND SOUTH CHINA SEA</title><title>Chinese journal of oceanology and limnology</title><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><description>OCCAM global ocean model results were applied to calculate the monthly water transport through 7 straits around the East China Sea(ECS)and the South china Sea(SCS).Analysis of the features of velocity profiles and their variations in the Togara Strait,Luzon Strait and Eastern Taiwan Strait showed that;1)the velocity profiles had striped pattern in the Eastern Taiwan Strait,where monthly flux varied from 22.4 to 28.1 Sv and annual mean was about 25.8 Sv;2)the profiles of velocity in the Togara Strait were characterized by core structure,and monthly flux varied from 23.3 to 31.4 Sv,with annual mean of about 27.9 Sv;3)water flowed from the SCS to the ECS in the Taiwan Strait,with maximum flux of 3.1 Sv in July and minimum of 0.9 Sv in November;4)the flux in the Tsushima Strait varied by only about 0.4 Sv by season and its annual mean was about 2.3 Sv;5)Kuroshio water flowed into the SCS in the Luzon Strait throughout the year and the velocity profiles were characterized by multi-core structure.The flux in the Luzon Strait was minimun in June(about 2.4 Sv)and maximum in February(about 9.0 Sv),and its annual mean was 4.8 Sv;6)the monthly flux in the Mindoro Strait was maximum in December(3.0 Sv)and minimum in June(Only 0.1 Sv),and its annual mean was 1.3 Sv;7)Karimata Strait water flowed into the SCS from May to August,with maximum in-flow flux of about 0.75 Sv in June and flowed out from September to April at maximum outflow flux of 3.9 Sv in January.The annual mean flux was about 1.35 Sv.</description><subject>Annual</subject><subject>Fluctuations</subject><subject>Inflow</subject><subject>Marine</subject><subject>Monthly</subject><subject>Ocean circulation</subject><subject>Ocean models</subject><subject>Oceanography</subject><subject>Outflow</subject><subject>Straits</subject><subject>Studies</subject><subject>Velocity</subject><subject>Velocity distribution</subject><subject>Velocity profiles</subject><subject>Water</subject><subject>Water transport</subject><subject>Waterways</subject><issn>0254-4059</issn><issn>2096-5508</issn><issn>1993-5005</issn><issn>2523-3521</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNp10d1KwzAUB_AgCs7pjU8QFQSF6knSNs1lnZ0d6Cprhnhj6GKyTWerrcOPKx_CJ_RJjEwUBK9ySH78DycHoU0CBwSAHx51gUY-FyRaQi0iBPMCgGAZtYAGvudDIFbRWtPcADDhg2ihq1wOjy9x1sUXsUwGH2_vchD38_NsILFMB9nwJMV5dpbgs7jXx7l77Mkcu1KmCU7iXOJO2uvHOE9iHPePnR3K9PduHa3YYtaYje-zjYbdRHZS7zQ76XXiU09TSonH7XUwYpYIBoTRSAsRimtr_RHxKTGF1tpEjPvCiIhqOio0IQIM44wXjFtXtdHeIvepKG1RjtVNNa9L11G9jicvk9fnEQWg4IPLb6Pdhb2vq4e5aR7V3bTRZjYrSlPNG0Ui91ksCB3c-QN_UqkgXIRRKLhT2_8qCFwUYV899xdI11XT1Maq-3p6V9QvioD62pz63ZzDW994UpXjh6kbx418a6czo3hIwjCI2CfVEYut</recordid><startdate>20021201</startdate><enddate>20021201</enddate><creator>鲍献文 高郭平 吴德星</creator><general>Springer Nature B.V</general><general>Dept. of Oceanography, Ocean University of Qingdao, Qingdao 266003,China</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7QL</scope><scope>7SN</scope><scope>7TN</scope><scope>7U7</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>M7N</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20021201</creationdate><title>STUDY OF WATER—TRANSPORT THROUGH SOME MAIN STRAITS IN THE EAST CHINA SEA AND SOUTH CHINA SEA</title><author>鲍献文 高郭平 吴德星</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2221-7fd5b3f19301328c9969dff4b1421eaccce83749e982c2bac1190e3737a37f0e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Annual</topic><topic>Fluctuations</topic><topic>Inflow</topic><topic>Marine</topic><topic>Monthly</topic><topic>Ocean circulation</topic><topic>Ocean models</topic><topic>Oceanography</topic><topic>Outflow</topic><topic>Straits</topic><topic>Studies</topic><topic>Velocity</topic><topic>Velocity distribution</topic><topic>Velocity profiles</topic><topic>Water</topic><topic>Water transport</topic><topic>Waterways</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>鲍献文 高郭平 吴德星</creatorcontrib><collection>维普_期刊</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>维普中文期刊数据库</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Toxicology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Science Journals</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Chinese journal of oceanology and limnology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>鲍献文 高郭平 吴德星</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>STUDY OF WATER—TRANSPORT THROUGH SOME MAIN STRAITS IN THE EAST CHINA SEA AND SOUTH CHINA SEA</atitle><jtitle>Chinese journal of oceanology and limnology</jtitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><date>2002-12-01</date><risdate>2002</risdate><volume>20</volume><issue>4</issue><spage>293</spage><epage>302</epage><pages>293-302</pages><issn>0254-4059</issn><issn>2096-5508</issn><eissn>1993-5005</eissn><eissn>2523-3521</eissn><abstract>OCCAM global ocean model results were applied to calculate the monthly water transport through 7 straits around the East China Sea(ECS)and the South china Sea(SCS).Analysis of the features of velocity profiles and their variations in the Togara Strait,Luzon Strait and Eastern Taiwan Strait showed that;1)the velocity profiles had striped pattern in the Eastern Taiwan Strait,where monthly flux varied from 22.4 to 28.1 Sv and annual mean was about 25.8 Sv;2)the profiles of velocity in the Togara Strait were characterized by core structure,and monthly flux varied from 23.3 to 31.4 Sv,with annual mean of about 27.9 Sv;3)water flowed from the SCS to the ECS in the Taiwan Strait,with maximum flux of 3.1 Sv in July and minimum of 0.9 Sv in November;4)the flux in the Tsushima Strait varied by only about 0.4 Sv by season and its annual mean was about 2.3 Sv;5)Kuroshio water flowed into the SCS in the Luzon Strait throughout the year and the velocity profiles were characterized by multi-core structure.The flux in the Luzon Strait was minimun in June(about 2.4 Sv)and maximum in February(about 9.0 Sv),and its annual mean was 4.8 Sv;6)the monthly flux in the Mindoro Strait was maximum in December(3.0 Sv)and minimum in June(Only 0.1 Sv),and its annual mean was 1.3 Sv;7)Karimata Strait water flowed into the SCS from May to August,with maximum in-flow flux of about 0.75 Sv in June and flowed out from September to April at maximum outflow flux of 3.9 Sv in January.The annual mean flux was about 1.35 Sv.</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1007/BF02847918</doi><tpages>10</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0254-4059 |
ispartof | Chinese journal of oceanology and limnology, 2002-12, Vol.20 (4), p.293-302 |
issn | 0254-4059 2096-5508 1993-5005 2523-3521 |
language | eng |
recordid | cdi_wanfang_journals_zghyhzxb200204001 |
source | Springer Link |
subjects | Annual Fluctuations Inflow Marine Monthly Ocean circulation Ocean models Oceanography Outflow Straits Studies Velocity Velocity distribution Velocity profiles Water Water transport Waterways |
title | STUDY OF WATER—TRANSPORT THROUGH SOME MAIN STRAITS IN THE EAST CHINA SEA AND SOUTH CHINA SEA |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-24T07%3A30%3A51IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wanfang_jour_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=STUDY%20OF%20WATER%E2%80%94TRANSPORT%20THROUGH%20SOME%20MAIN%20STRAITS%20IN%20THE%20EAST%20CHINA%20SEA%20AND%20SOUTH%20CHINA%20SEA&rft.jtitle=Chinese%20journal%20of%20oceanology%20and%20limnology&rft.au=%E9%B2%8D%E7%8C%AE%E6%96%87%20%E9%AB%98%E9%83%AD%E5%B9%B3%20%E5%90%B4%E5%BE%B7%E6%98%9F&rft.date=2002-12-01&rft.volume=20&rft.issue=4&rft.spage=293&rft.epage=302&rft.pages=293-302&rft.issn=0254-4059&rft.eissn=1993-5005&rft_id=info:doi/10.1007/BF02847918&rft_dat=%3Cwanfang_jour_proqu%3Ezghyhzxb200204001%3C/wanfang_jour_proqu%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c2221-7fd5b3f19301328c9969dff4b1421eaccce83749e982c2bac1190e3737a37f0e3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=205025131&rft_id=info:pmid/&rft_cqvip_id=7616658&rft_wanfj_id=zghyhzxb200204001&rfr_iscdi=true |