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contributor authorMachín, Francisco
contributor authorPelegrí, Josep L.
contributor authorFraile-Nuez, E.
contributor authorVélez-Belchí, P.
contributor authorLópez-Laatzen, F.
contributor authorHernández-Guerra, A.
date accessioned2017-06-09T16:36:43Z
date available2017-06-09T16:36:43Z
date copyright2010/08/01
date issued2010
identifier issn0022-3670
identifier otherams-70918.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212752
description abstractTwo 9-yr current-meter and salinity records, together with climatological data, reveal marked seasonal variability of the intermediate flow at a key location in the Canary Basin. The region is characterized by a summer (July?September) and early fall (October) northward progression of Antarctic Intermediate Water followed by a fall (November?December) intense flow reversal of Mediterranean Water. A Sverdrup-type model confirms that these movements are associated with stretching or shrinking of the intermediate water strata.
publisherAmerican Meteorological Society
titleSeasonal Flow Reversals of Intermediate Waters in the Canary Current System East of the Canary Islands
typeJournal Paper
journal volume40
journal issue8
journal titleJournal of Physical Oceanography
identifier doi10.1175/2010JPO4320.1
journal fristpage1902
journal lastpage1909
treeJournal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 008
contenttypeFulltext


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