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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 22, issue 12
Ann. Geophys., 22, 4043–4048, 2004
https://doi.org/10.5194/angeo-22-4043-2004
© Author(s) 2004. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 22, 4043–4048, 2004
https://doi.org/10.5194/angeo-22-4043-2004
© Author(s) 2004. This work is distributed under
the Creative Commons Attribution 3.0 License.

  22 Dec 2004

22 Dec 2004

Surface winds in the Euro-Mediterranean area: the real resolution of numerical grids

F. Chèruy1, A. Speranza2, A. Sutera3, and N. Tartaglione4 F. Chèruy et al.
  • 1Laboratoire de Météorologie Dynamique, CNRS, Paris, France
  • 2Department of Mathematics and Informatics, University of Camerino, Camerino, Italy
  • 3Department of Physics, University "La Sapienza", Rome, Italy
  • 4Department of Physics, University of Camerino, Camerino, Italy

Abstract. Surface wind is a variable of great importance in forcing marine waves and circulations, modulating surface fluxes, etc. Surface wind defined on numerical grids is currently used in forecast-analysis, as well as in climatology. Gridded fields, however, suffer for systematic errors associated with the numerical procedures adopted in computing them. In this paper the climatology of surface wind produced by three different numerical models in the European-Mediterranean area is analyzed. The systematic loss of power at the smallest grid-scales appears in the power spectrum of all the different models. Some prototype numerical integrations show that this systematic over-smoothing is due to numerical stabilization operators that represent the main source of the diagnosed error; the error progression in space and time is also analyzed.

Key words. Meteorology and atmospheric dynamics (Mesoscale meteorology; Ocean-atmosphere interaction; Climatology)

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