http://www.cnr.it/ontology/cnr/individuo/prodotto/ID173489
The role of surface fluxes in OGCM using satellite SST. Validation of and sensitivity to the forcing frequency of the Mediterranean thermohaline circulation (Articolo in rivista)
- Type
- Label
- The role of surface fluxes in OGCM using satellite SST. Validation of and sensitivity to the forcing frequency of the Mediterranean thermohaline circulation (Articolo in rivista) (literal)
- Anno
- 2002-01-01T00:00:00+01:00 (literal)
- Alternative label
Artale V., Iudicone D., Santoleri R., Rupolo V., Marullo S., D'Ortenzio F. (2002)
The role of surface fluxes in OGCM using satellite SST. Validation of and sensitivity to the forcing frequency of the Mediterranean thermohaline circulation
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Artale V., Iudicone D., Santoleri R., Rupolo V., Marullo S., D'Ortenzio F. (literal)
- Pagina inizio
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- Volume 107 (C8), doi:10.1029/2000JC000452 doi:10.1029/2000JC000452 (literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Titolo
- The role of surface fluxes in OGCM using satellite SST. Validation of and sensitivity to the forcing frequency of the Mediterranean thermohaline circulation (literal)
- Abstract
- In this article we study the effect of high frequency surface momentum and
heat fluxes in the numerical simulation of some key ocean processes of the
Mediterranean thermohaline circulation. The lack of synoptic and
reliable heat and freshwater flux datasets is bypassed using the relaxation
approach both for the salinity and temperature surface field. We propose a
parameterization of the heat fluxes in which the temperature restoring
coefficient depends on wind intensity and regime and that requires the use
of simuoultaneous satellite daily SST estimates as restoring field. The
consistency of the proposed parameterization and of its numerical
implementation with the previous oceanic boundary layer studies has been
verified trough the analysis of the Saunders proportionality constant.
This parameterization coupling simultaneous surface heat fluxes and wind
trough the skin-bulk temperature difference, recovers the high variability
of the air-sea exchanges of the extreme events in the Mediterranean sea.
The effect of high frequency surface momentum and heat fluxes is studied
comparing results from two different experiments forced with monthly and
daily surface wind and satellite SST data sets. This comparisons show the
relevance of high frequency forcing in the representation of the dynamical
processes relative to the intermediate water mass transformation and
horizontal advection as well as in the deep water formation in the
north-western Mediterranean Sea. (literal)
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