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contributor authorPrater, Mark D.
contributor authorSanford, Thomas B.
date accessioned2017-06-09T14:51:07Z
date available2017-06-09T14:51:07Z
date copyright1994/07/01
date issued1994
identifier issn0022-3670
identifier otherams-28184.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165272
description abstractA meddy, an eddy formed from Mediterranean source water, was surveyed in detail with two types of expendable profilers and a CTD instrument. The muddy comprised two distinct, vertically aligned tenses with a combined thickness of 650 m. Both lenses were stratification minima. The upper lens was warmer, fresher (12.25°C, 36.5 psu), and more circular., the lower lens was cooler, more saline (12.1°C, 36.65 psu), and more elliptical, oriented alone a northeast by southwest line. The upper lens, homogeneous out to a radius of 6 km, had a radius of maximum velocity of 9 km. Its relative vorticity was ?0.85 f, and its Ertel potential vorticity, 4 ? 10?12 (m s)?1, was 17 times below ambient levels due to the combined effects of negative relative vorticity and vortex stretching. The meddy contained more kinetic energy than available potential energy (energy Burger number of 2.5). Compared with historical meddies, it had a larger Burger number and a more negative vorticity Rossby number.
publisherAmerican Meteorological Society
titleA Meddy off Cape St. Vincent. Part I: Description
typeJournal Paper
journal volume24
journal issue7
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1994)024<1572:AMOCSV>2.0.CO;2
journal fristpage1572
journal lastpage1586
treeJournal of Physical Oceanography:;1994:;Volume( 024 ):;issue: 007
contenttypeFulltext


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