The general circulation in the Mediterranean Sea: a climatological approach

Citation
Jm. Brankart et P. Brasseur, The general circulation in the Mediterranean Sea: a climatological approach, J MAR SYST, 18(1-3), 1998, pp. 41-70
Citations number
39
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
JOURNAL OF MARINE SYSTEMS
ISSN journal
09247963 → ACNP
Volume
18
Issue
1-3
Year of publication
1998
Pages
41 - 70
Database
ISI
SICI code
0924-7963(199812)18:1-3<41:TGCITM>2.0.ZU;2-Q
Abstract
A significant amount of hydrographic data has been collected in the Mediter ranean during this century, providing the basic ingredients needed to const ruct a climatological picture of the general circulation. A pooled hydrogra phic data set has been prepared, which currently contains over 100,000 stat ion profiles (CTD, Nansen bottle, XBT and MET) taken in the Eastern and Wes tern Mediterranean Sea between 1900 and 1993. Climatological analyses of te mperature and salinity data are performed at seasonal and monthly scales, u sing a variational method and a finite element numerical technique. The var iational formulation had been demonstrated to be equivalent to objective an alysis, and a hybridation of the statistical and variational methods allows to compute error fields associated to the climatology. The free parameters of the scheme are determined using a cross-validation algorithm to extract the best seasonal statistics from the observed data sets. Compared to earl ier climatologies, the recent analyses show significant improvements with r espect to the regional scales of the general circulation gyres. In addition , several features of the general circulation are described with a better a ccuracy. Finally, the barotropic equations (external mode) of a free-surfac e, primitive equation model are integrated in time to diagnostically adjust the sea-surface elevation to the thermohaline structures. Geostrophic velo cities are then computed, integrating the thermal-wind equations with the s ea-surface pressure as a reference. Results of fully prognostic, three-dime nsional, primitive equation models are compared with these diagnostic compu tations in order to identify which features of the general circulation can be captured by observations. (C) 1998 Elsevier Science B.V. All rights rese rved.