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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2003-01-01
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Series: | Annales Geophysicae |
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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 |
work_keys_str_mv |
AT rsorgente seasonalvariabilityinthecentralmediterraneanseacirculation AT afdrago seasonalvariabilityinthecentralmediterraneanseacirculation AT aribotti seasonalvariabilityinthecentralmediterraneanseacirculation |
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