Two decades of mesoscale phenomena on either side of the Strait of Gibraltar

Mesoscale circulation patterns in the adjacent basins of the Strait of Gibraltar were investigated by means of altimetry data. In the Gulf of Cádiz, the pattern is relatively stable with two gyres: a cyclonic gyre close to the southern Iberian coast and an anticyclonic one on the western side of the...

Full description

Bibliographic Details
Main Authors: Javier Delgado, Jesús García-Lafuente, Cristina Naranjo
Format: Article
Language:English
Published: Consejo Superior de Investigaciones Científicas 2012-09-01
Series:Scientia Marina
Subjects:
Online Access:http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/1377
id doaj-eb11807919b3424f835562c1118154d1
record_format Article
spelling doaj-eb11807919b3424f835562c1118154d12021-05-05T13:49:37ZengConsejo Superior de Investigaciones CientíficasScientia Marina0214-83581886-81342012-09-0176S19510210.3989/scimar.03609.18E1362Two decades of mesoscale phenomena on either side of the Strait of GibraltarJavier Delgado0Jesús García-Lafuente1Cristina Naranjo2Department of Applied Physics II, University of Málaga, Campus de Excelencia Internacional del Mar (CEI·MAR)Department of Applied Physics II, University of Málaga, Campus de Excelencia Internacional del Mar (CEI·MAR)Department of Applied Physics II, University of Málaga, Campus de Excelencia Internacional del Mar (CEI·MAR)Mesoscale circulation patterns in the adjacent basins of the Strait of Gibraltar were investigated by means of altimetry data. In the Gulf of Cádiz, the pattern is relatively stable with two gyres: a cyclonic gyre close to the southern Iberian coast and an anticyclonic one on the western side of the Strait of Gibraltar. Both structures are located in the right place to convey the surface circulation towards the Strait and feed the Atlantic inflow. In the Alboran Sea, our results confirm that the western anticyclonic gyre is the most stable feature observed, while the eastern cyclonic gyre is subject to great variability. The mesoscale structures fluctuate at seasonal and interannual frequencies, but they may also undergo great changes in a very short time scale. A simple correlation analysis suggests that changes in the upstream Gulf of Cádiz basin may be transmitted through the Strait of Gibraltar to the Alboran Sea with a time delay of around one week.http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/1377satellite altimetrymesoscale circulation patternsseasonal variabilityinterannual variabilitystrait of gibraltargulf of cádizalboran sea
collection DOAJ
language English
format Article
sources DOAJ
author Javier Delgado
Jesús García-Lafuente
Cristina Naranjo
spellingShingle Javier Delgado
Jesús García-Lafuente
Cristina Naranjo
Two decades of mesoscale phenomena on either side of the Strait of Gibraltar
Scientia Marina
satellite altimetry
mesoscale circulation patterns
seasonal variability
interannual variability
strait of gibraltar
gulf of cádiz
alboran sea
author_facet Javier Delgado
Jesús García-Lafuente
Cristina Naranjo
author_sort Javier Delgado
title Two decades of mesoscale phenomena on either side of the Strait of Gibraltar
title_short Two decades of mesoscale phenomena on either side of the Strait of Gibraltar
title_full Two decades of mesoscale phenomena on either side of the Strait of Gibraltar
title_fullStr Two decades of mesoscale phenomena on either side of the Strait of Gibraltar
title_full_unstemmed Two decades of mesoscale phenomena on either side of the Strait of Gibraltar
title_sort two decades of mesoscale phenomena on either side of the strait of gibraltar
publisher Consejo Superior de Investigaciones Científicas
series Scientia Marina
issn 0214-8358
1886-8134
publishDate 2012-09-01
description Mesoscale circulation patterns in the adjacent basins of the Strait of Gibraltar were investigated by means of altimetry data. In the Gulf of Cádiz, the pattern is relatively stable with two gyres: a cyclonic gyre close to the southern Iberian coast and an anticyclonic one on the western side of the Strait of Gibraltar. Both structures are located in the right place to convey the surface circulation towards the Strait and feed the Atlantic inflow. In the Alboran Sea, our results confirm that the western anticyclonic gyre is the most stable feature observed, while the eastern cyclonic gyre is subject to great variability. The mesoscale structures fluctuate at seasonal and interannual frequencies, but they may also undergo great changes in a very short time scale. A simple correlation analysis suggests that changes in the upstream Gulf of Cádiz basin may be transmitted through the Strait of Gibraltar to the Alboran Sea with a time delay of around one week.
topic satellite altimetry
mesoscale circulation patterns
seasonal variability
interannual variability
strait of gibraltar
gulf of cádiz
alboran sea
url http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/1377
work_keys_str_mv AT javierdelgado twodecadesofmesoscalephenomenaoneithersideofthestraitofgibraltar
AT jesusgarcialafuente twodecadesofmesoscalephenomenaoneithersideofthestraitofgibraltar
AT cristinanaranjo twodecadesofmesoscalephenomenaoneithersideofthestraitofgibraltar
_version_ 1721461130035986432