Hindcasting turbulent properties in the upper layers of the southern Adriatic Sea by means of GOTM and the GHER 1-D model (Contributo in atti di convegno)

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  • Hindcasting turbulent properties in the upper layers of the southern Adriatic Sea by means of GOTM and the GHER 1-D model (Contributo in atti di convegno) (literal)
Anno
  • 2007-01-01T00:00:00+01:00 (literal)
Alternative label
  • Lenartz F. (1), Barth A. (2), Carniel S. (3), Kantha L. (4), Rixen M. (5), Vandenbulcke L. (1), Beckers J.-M. (1) (2007)
    Hindcasting turbulent properties in the upper layers of the southern Adriatic Sea by means of GOTM and the GHER 1-D model
    in 39th International Liège Colloquium on Ocean Dynamics and 3rd Warnemuende Turbulence Days, Liège, Belgium
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Lenartz F. (1), Barth A. (2), Carniel S. (3), Kantha L. (4), Rixen M. (5), Vandenbulcke L. (1), Beckers J.-M. (1) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
  • http://modb.oce.ulg.ac.be/colloquium/2007abstracts.pdf http://modb.oce.ulg.ac.be/colloquium/2007.html (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#descrizioneSinteticaDelProdotto
  • Part of the DART06-A and -B observational campaigns, carried out by the NRV Alliance in March and August 2006 in the southern Adriatic Sea, consisted in turbulence measurements by means of a microstructure profiler. A very high number of casts were made in a location where a long-term mooring deployed at 90 m deep provided us with temperature, salinity and velocity profiles. In addition, meteorological and surface wave conditions were also collected at this point. Turbulent properties in the upper layer were measured under a variety of atmospheric forcings, including strong wind, nighttime convection, regular wind and mixed convection, as well as weak wind and strong isolation conditions. This large dataset constitutes a great opportunity to validate, test and possibly improve existing hydrodynamic models. We thus have performed numerous simulations with GOTM [Burhcard and Bolding, 2000] – the well-known General Ocean Turbulence Model – and the GHER [Beckers, 1991] – GeoHydrodynamics and Environmental Research – 1-D model. On one hand, we have compared the outputs with the turbulent properties derived from the measurements, and on the other hand, with the outputs of each other. We have performed a lot of error analyses to characterize and explain the differences. (literal)
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  • (1) University of Liège, Belgium (2) University of Florida, USA (3) CNR-ISMAR, Italy (4) University of Colorador, USA (5) NURC, Italy (literal)
Titolo
  • Hindcasting turbulent properties in the upper layers of the southern Adriatic Sea by means of GOTM and the GHER 1-D model (literal)
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