Seasonal variability in the Central Mediterranean Sea circulation

A high resolution eddy-resolving primitive equation numerical model, based on the Princeton Ocean Model (POM), is used to study the seasonal variability of the general circulation in the Central Mediterranean Sea. The model is run on a seasonal cycle, perpetual year simulation for five years...

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Main Authors: R. Sorgente, A. F. Drago, A. Ribotti
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/21/299/2003/angeo-21-299-2003.pdf
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spelling doaj-6bcf303625834a658b90f054660e826d2020-11-24T21:02:28ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762003-01-012129932210.5194/angeo-21-299-2003Seasonal variability in the Central Mediterranean Sea circulationR. Sorgente0A. F. Drago1A. Ribotti2CNR-IAMC, Sect. Oristano, c/o International Marine Centre, Loc. Sa Mardini, 09072 Torregrande-Oristano, ItalyPhysical Oceanography Unit, IOI-MOC, University of Malta, c/o 36, Old Mint Str., Valletta VLT12, MaltaCNR-IAMC, Sect. Oristano, c/o International Marine Centre, Loc. Sa Mardini, 09072 Torregrande-Oristano, ItalyA high resolution eddy-resolving primitive equation numerical model, based on the Princeton Ocean Model (POM), is used to study the seasonal variability of the general circulation in the Central Mediterranean Sea. The model is run on a seasonal cycle, perpetual year simulation for five years, with nesting to the coarser resolution Ocean General Circulation Model (OGCM), covering the whole Mediterranean Sea. The model results are compared to the current knowledge on the hydrography and dynamics of the area, with a special focus on the annual cycle of the Modified Atlantic Water (MAW), on the circulation in the Sardinia Channel, the water exchange across the Strait of Sicily, and on the transition and fate of the Levantine Intermediate Water (LIW). The results show that the adopted coupling techniques between the two models give a proficient downscaling of the large-scale OGCM flow field into the regional scale model. The numerical solution is also used to highlight the seasonal characteristics of important dynamical features in the area, as well as to shed light on the scarcely known circulation regimes along the north African shelf and slope.<br><br> <b>Key words. </b>Oceanography: general (numerical modelling); Oceanography: physical (currents; general circulation)https://www.ann-geophys.net/21/299/2003/angeo-21-299-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. Sorgente
A. F. Drago
A. Ribotti
spellingShingle R. Sorgente
A. F. Drago
A. Ribotti
Seasonal variability in the Central Mediterranean Sea circulation
Annales Geophysicae
author_facet R. Sorgente
A. F. Drago
A. Ribotti
author_sort R. Sorgente
title Seasonal variability in the Central Mediterranean Sea circulation
title_short Seasonal variability in the Central Mediterranean Sea circulation
title_full Seasonal variability in the Central Mediterranean Sea circulation
title_fullStr Seasonal variability in the Central Mediterranean Sea circulation
title_full_unstemmed Seasonal variability in the Central Mediterranean Sea circulation
title_sort seasonal variability in the central mediterranean sea circulation
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2003-01-01
description A high resolution eddy-resolving primitive equation numerical model, based on the Princeton Ocean Model (POM), is used to study the seasonal variability of the general circulation in the Central Mediterranean Sea. The model is run on a seasonal cycle, perpetual year simulation for five years, with nesting to the coarser resolution Ocean General Circulation Model (OGCM), covering the whole Mediterranean Sea. The model results are compared to the current knowledge on the hydrography and dynamics of the area, with a special focus on the annual cycle of the Modified Atlantic Water (MAW), on the circulation in the Sardinia Channel, the water exchange across the Strait of Sicily, and on the transition and fate of the Levantine Intermediate Water (LIW). The results show that the adopted coupling techniques between the two models give a proficient downscaling of the large-scale OGCM flow field into the regional scale model. The numerical solution is also used to highlight the seasonal characteristics of important dynamical features in the area, as well as to shed light on the scarcely known circulation regimes along the north African shelf and slope.<br><br> <b>Key words. </b>Oceanography: general (numerical modelling); Oceanography: physical (currents; general circulation)
url https://www.ann-geophys.net/21/299/2003/angeo-21-299-2003.pdf
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