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...
Published in: | Journal of Physical Oceanography |
---|---|
Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , |
Language: | English |
Published: |
0022-3670
2010
|
Subjects: | |
Online Access: | http://hdl.handle.net/10553/49043 https://doi.org/10.1175/2010JPO4320.1 |
_version_ | 1821757082124156928 |
---|---|
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 |
id | ftunivlaspalmas:oai:https://accedacris.ulpgc.es:10553/49043 |
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 78049318509 000281520800015 1909 1902 40 WOS:000281520800015 D-1521-2010 I-9150-2017 L-5815-2014 A-9287-2009 A-4747-2008 |
op_source | Journal of Physical Oceanography [ISSN 0022-3670], v. 40, p. 1902-1909 |
publishDate | 2010 |
publisher | 0022-3670 |
record_format | openpolar |
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 |