Seasonal flow reversals of intermediate waters in the canary current system east of the canary Islands

Two 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 Inte...

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Published in:Journal of Physical Oceanography
Main Authors: Machín, Francisco, Pelegrí, Josep L., Fraile-Nuez, E., Vélez-Belchí, P., López-Laatzen, F., Hernández-Guerra, A.
Other Authors: Fraile-Nuez, Eugenio, Velez-Belchi, Pedro, Pelegri, Josep, Machin, Francisco, Hernandez-Guerra, Alonso, 6602804374, 7003869003, 12139561900, 7801599223, 6506580233, 6701736545, 1451397, 358123, 1139939, 1378362, 5387532, 660191
Language:English
Published: 0022-3670 2010
Subjects:
Online Access:http://hdl.handle.net/10553/49043
https://doi.org/10.1175/2010JPO4320.1
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author Machín, Francisco
Pelegrí, Josep L.
Fraile-Nuez, E.
Vélez-Belchí, P.
López-Laatzen, F.
Hernández-Guerra, A.
author2 Fraile-Nuez, Eugenio
Velez-Belchi, Pedro
Pelegri, Josep
Machin, Francisco
Hernandez-Guerra, Alonso
6602804374
7003869003
12139561900
7801599223
6506580233
6701736545
1451397
358123
1139939
1378362
5387532
660191
author_facet Machín, Francisco
Pelegrí, Josep L.
Fraile-Nuez, E.
Vélez-Belchí, P.
López-Laatzen, F.
Hernández-Guerra, A.
author_sort Machín, Francisco
collection Universidad de Las Palmas de Gran Canaria: Acceda
container_issue 8
container_start_page 1902
container_title Journal of Physical Oceanography
container_volume 40
description Two 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.
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
geographic Antarctic
geographic_facet Antarctic
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institution Open Polar
language English
op_collection_id ftunivlaspalmas
op_container_end_page 1909
op_doi https://doi.org/10.1175/2010JPO4320.1
op_relation Ctm2005-04701-C02-02-01/Mar. Origen de la Corriente de Canarias.
Journal of Physical Oceanography
0022-3670
http://hdl.handle.net/10553/49043
doi:10.1175/2010JPO4320.1
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op_source Journal of Physical Oceanography [ISSN 0022-3670], v. 40, p. 1902-1909
publishDate 2010
publisher 0022-3670
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spelling ftunivlaspalmas:oai:https://accedacris.ulpgc.es:10553/49043 2025-01-16T19:25:40+00:00 Seasonal flow reversals of intermediate waters in the canary current system east of the canary Islands Machín, Francisco Pelegrí, Josep L. Fraile-Nuez, E. Vélez-Belchí, P. López-Laatzen, F. Hernández-Guerra, A. Fraile-Nuez, Eugenio Velez-Belchi, Pedro Pelegri, Josep Machin, Francisco Hernandez-Guerra, Alonso 6602804374 7003869003 12139561900 7801599223 6506580233 6701736545 1451397 358123 1139939 1378362 5387532 660191 2010 http://hdl.handle.net/10553/49043 https://doi.org/10.1175/2010JPO4320.1 eng eng 0022-3670 Ctm2005-04701-C02-02-01/Mar. Origen de la Corriente de Canarias. Journal of Physical Oceanography 0022-3670 http://hdl.handle.net/10553/49043 doi:10.1175/2010JPO4320.1 78049318509 000281520800015 1909 1902 40 WOS:000281520800015 D-1521-2010 I-9150-2017 L-5815-2014 A-9287-2009 A-4747-2008 Journal of Physical Oceanography [ISSN 0022-3670], v. 40, p. 1902-1909 Investigación Seasonal variability Intermediate waters Salinity Currents 2010 ftunivlaspalmas https://doi.org/10.1175/2010JPO4320.1 2020-01-01T00:07:47Z Two 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. Other/Unknown Material Antarc* Antarctic Universidad de Las Palmas de Gran Canaria: Acceda Antarctic Journal of Physical Oceanography 40 8 1902 1909
spellingShingle Investigación
Seasonal variability
Intermediate waters
Salinity
Currents
Machín, Francisco
Pelegrí, Josep L.
Fraile-Nuez, E.
Vélez-Belchí, P.
López-Laatzen, F.
Hernández-Guerra, A.
Seasonal flow reversals of intermediate waters in the canary current system east of the canary Islands
title Seasonal flow reversals of intermediate waters in the canary current system east of the canary Islands
title_full Seasonal flow reversals of intermediate waters in the canary current system east of the canary Islands
title_fullStr Seasonal flow reversals of intermediate waters in the canary current system east of the canary Islands
title_full_unstemmed Seasonal flow reversals of intermediate waters in the canary current system east of the canary Islands
title_short Seasonal flow reversals of intermediate waters in the canary current system east of the canary Islands
title_sort seasonal flow reversals of intermediate waters in the canary current system east of the canary islands
topic Investigación
Seasonal variability
Intermediate waters
Salinity
Currents
topic_facet Investigación
Seasonal variability
Intermediate waters
Salinity
Currents
url http://hdl.handle.net/10553/49043
https://doi.org/10.1175/2010JPO4320.1