On the Cascading of Dense Shelf Waters in the Irminger SeaSource: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 012::page 2254Author:Falina, Anastasia
,
Sarafanov, Artem
,
Mercier, Herlé
,
Lherminier, Pascale
,
Sokov, Alexey
,
Daniault, Nathalie
DOI: 10.1175/JPO-D-12-012.1Publisher: American Meteorological Society
Abstract: ydrographic data collected in the Irminger Sea in the 1990s?2000s indicate that dense shelf waters carried by the East Greenland Current south of the Denmark Strait intermittently descend (cascade) down the continental slope and merge with the deep waters originating from the Nordic Seas overflows. Repeat measurements on the East Greenland shelf at ~200 km south of the Denmark Strait (65°?66°N) reveal that East Greenland shelf waters in the Irminger Sea are occasionally as dense (σ0 > 27.80) as the overflow-derived deep waters carried by the Deep Western Boundary Current (DWBC). Clear hydrographic traces of upstream cascading of dense shelf waters are found over the continental slope at 64.3°N, where the densest plumes (σ0 > 27.80) originating from the shelf are identified as distinct low-salinity anomalies in the DWBC. Downstream observations suggest that dense fresh waters descending from the shelf in the northern Irminger Sea can be distinguished in the DWBC up to the latitude of Cape Farewell (~60°N) and that these waters make a significant contribution to the DWBC transport.
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contributor author | Falina, Anastasia | |
contributor author | Sarafanov, Artem | |
contributor author | Mercier, Herlé | |
contributor author | Lherminier, Pascale | |
contributor author | Sokov, Alexey | |
contributor author | Daniault, Nathalie | |
date accessioned | 2017-06-09T17:19:32Z | |
date available | 2017-06-09T17:19:32Z | |
date copyright | 2012/12/01 | |
date issued | 2012 | |
identifier issn | 0022-3670 | |
identifier other | ams-83199.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4226397 | |
description abstract | ydrographic data collected in the Irminger Sea in the 1990s?2000s indicate that dense shelf waters carried by the East Greenland Current south of the Denmark Strait intermittently descend (cascade) down the continental slope and merge with the deep waters originating from the Nordic Seas overflows. Repeat measurements on the East Greenland shelf at ~200 km south of the Denmark Strait (65°?66°N) reveal that East Greenland shelf waters in the Irminger Sea are occasionally as dense (σ0 > 27.80) as the overflow-derived deep waters carried by the Deep Western Boundary Current (DWBC). Clear hydrographic traces of upstream cascading of dense shelf waters are found over the continental slope at 64.3°N, where the densest plumes (σ0 > 27.80) originating from the shelf are identified as distinct low-salinity anomalies in the DWBC. Downstream observations suggest that dense fresh waters descending from the shelf in the northern Irminger Sea can be distinguished in the DWBC up to the latitude of Cape Farewell (~60°N) and that these waters make a significant contribution to the DWBC transport. | |
publisher | American Meteorological Society | |
title | On the Cascading of Dense Shelf Waters in the Irminger Sea | |
type | Journal Paper | |
journal volume | 42 | |
journal issue | 12 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/JPO-D-12-012.1 | |
journal fristpage | 2254 | |
journal lastpage | 2267 | |
tree | Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 012 | |
contenttype | Fulltext |