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Meandering of the subtropical front south-east of the Azores
A subtropical front was observed in the area south and southeast of the Azores during cruises of FS Meteor and FS Poseidon in early 1982. The front has a basically west–east extension, with considerable meandering observed. Meso-scale eddies are found on both sides. The overall flow pattern correspo...
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Published in: | Nature (London) 1982-11, Vol.300 (5889), p.245-246 |
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container_end_page | 246 |
container_issue | 5889 |
container_start_page | 245 |
container_title | Nature (London) |
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creator | Käse, R. H Siedler, G |
description | A subtropical front was observed in the area south and southeast of the Azores during cruises of FS
Meteor
and FS
Poseidon
in early 1982. The front has a basically west–east extension, with considerable meandering observed. Meso-scale eddies are found on both sides. The overall flow pattern corresponds to earlier results on geopotential differences in the upper northeast Atlantic, but the baroclinic transport of the order of 10
7
m
3
s
−1
is found to be concentrated in a 60-km wide jet. We suggest here that the current band is part of the gyre circulation, resulting from a branching of the North Atlantic Current. |
doi_str_mv | 10.1038/300245a0 |
format | article |
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Meteor
and FS
Poseidon
in early 1982. The front has a basically west–east extension, with considerable meandering observed. Meso-scale eddies are found on both sides. The overall flow pattern corresponds to earlier results on geopotential differences in the upper northeast Atlantic, but the baroclinic transport of the order of 10
7
m
3
s
−1
is found to be concentrated in a 60-km wide jet. We suggest here that the current band is part of the gyre circulation, resulting from a branching of the North Atlantic Current.</description><identifier>ISSN: 0028-0836</identifier><identifier>EISSN: 1476-4687</identifier><identifier>DOI: 10.1038/300245a0</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>Humanities and Social Sciences ; letter ; multidisciplinary ; Science ; Science (multidisciplinary)</subject><ispartof>Nature (London), 1982-11, Vol.300 (5889), p.245-246</ispartof><rights>Springer Nature Limited 1982</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c1970-d24fdf6049e91727b793f89640675b6838b56dd1bf77ff221451228d41b45d073</citedby><cites>FETCH-LOGICAL-c1970-d24fdf6049e91727b793f89640675b6838b56dd1bf77ff221451228d41b45d073</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,2727,27924,27925</link.rule.ids></links><search><creatorcontrib>Käse, R. H</creatorcontrib><creatorcontrib>Siedler, G</creatorcontrib><title>Meandering of the subtropical front south-east of the Azores</title><title>Nature (London)</title><addtitle>Nature</addtitle><description>A subtropical front was observed in the area south and southeast of the Azores during cruises of FS
Meteor
and FS
Poseidon
in early 1982. The front has a basically west–east extension, with considerable meandering observed. Meso-scale eddies are found on both sides. The overall flow pattern corresponds to earlier results on geopotential differences in the upper northeast Atlantic, but the baroclinic transport of the order of 10
7
m
3
s
−1
is found to be concentrated in a 60-km wide jet. We suggest here that the current band is part of the gyre circulation, resulting from a branching of the North Atlantic Current.</description><subject>Humanities and Social Sciences</subject><subject>letter</subject><subject>multidisciplinary</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><issn>0028-0836</issn><issn>1476-4687</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1982</creationdate><recordtype>article</recordtype><recordid>eNptz0tLxDAUBeAgCtZR8BdIl7qI3rxTcDMMvmDEja5L2iROh7EZknShv94OdWbl6sLl43AOQpcEbgkwfccAKBcGjlBBuJKYS62OUTF-NQbN5Ck6S2kNAIIoXqD7V2d662LXf5bBl3nlyjQ0OYZt15pN6WPoc5nCkFfYmZT3Zv4Tokvn6MSbTXIXf3eGPh4f3hfPePn29LKYL3FLKgXYUu6tl8ArVxFFVaMq5nUlOUglGqmZboS0ljReKe8pJVwQSrXlpOHCgmIzdD3ltjGkFJ2vt7H7MvG7JlDvVtf71SO9mWja7ja5WK_DEPux3X_2arK9yUN0h9AD-AUHS18Q</recordid><startdate>19821118</startdate><enddate>19821118</enddate><creator>Käse, R. H</creator><creator>Siedler, G</creator><general>Nature Publishing Group UK</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>19821118</creationdate><title>Meandering of the subtropical front south-east of the Azores</title><author>Käse, R. H ; Siedler, G</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1970-d24fdf6049e91727b793f89640675b6838b56dd1bf77ff221451228d41b45d073</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1982</creationdate><topic>Humanities and Social Sciences</topic><topic>letter</topic><topic>multidisciplinary</topic><topic>Science</topic><topic>Science (multidisciplinary)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Käse, R. H</creatorcontrib><creatorcontrib>Siedler, G</creatorcontrib><collection>CrossRef</collection><jtitle>Nature (London)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Käse, R. H</au><au>Siedler, G</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Meandering of the subtropical front south-east of the Azores</atitle><jtitle>Nature (London)</jtitle><stitle>Nature</stitle><date>1982-11-18</date><risdate>1982</risdate><volume>300</volume><issue>5889</issue><spage>245</spage><epage>246</epage><pages>245-246</pages><issn>0028-0836</issn><eissn>1476-4687</eissn><abstract>A subtropical front was observed in the area south and southeast of the Azores during cruises of FS
Meteor
and FS
Poseidon
in early 1982. The front has a basically west–east extension, with considerable meandering observed. Meso-scale eddies are found on both sides. The overall flow pattern corresponds to earlier results on geopotential differences in the upper northeast Atlantic, but the baroclinic transport of the order of 10
7
m
3
s
−1
is found to be concentrated in a 60-km wide jet. We suggest here that the current band is part of the gyre circulation, resulting from a branching of the North Atlantic Current.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><doi>10.1038/300245a0</doi><tpages>2</tpages></addata></record> |
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ispartof | Nature (London), 1982-11, Vol.300 (5889), p.245-246 |
issn | 0028-0836 1476-4687 |
language | eng |
recordid | cdi_crossref_primary_10_1038_300245a0 |
source | Nature Journals Online |
subjects | Humanities and Social Sciences letter multidisciplinary Science Science (multidisciplinary) |
title | Meandering of the subtropical front south-east of the Azores |
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