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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 25, issue 3
Ann. Geophys., 25, 581–595, 2007
https://doi.org/10.5194/angeo-25-581-2007
© Author(s) 2007. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 25, 581–595, 2007
https://doi.org/10.5194/angeo-25-581-2007
© Author(s) 2007. This work is distributed under
the Creative Commons Attribution 3.0 License.

  29 Mar 2007

29 Mar 2007

Assimilation of radar altimeter data in numerical wave models: an impact study in two different wave climate regions

G. Emmanouil1, G. Galanis1,2, G. Kallos1, L. A. Breivik3, H. Heiberg3, and M. Reistad4 G. Emmanouil et al.
  • 1University of Athens, School of Physics, Division of Applied Physics, Atmospheric Modeling and Weather Forecasting Group, University Campus, Bldg. PHYS-V, 15784 Athens, Greece
  • 2Naval Academy of Greece, Section of Mathematics, Xatzikyriakion, 185 39, Piraeus, Greece
  • 3Norwegian Meteorological Institute, Research and Development Department, Section of Remote Sensing, POB 43 Blindern, 0313 Oslo, Norway
  • 4Norwegian Meteorological Institute, Forecasting Division of Western Norway, Allégaten 70, 5007 Bergen, 0313 Oslo, Norway

Abstract. An operational assimilation system incorporating significant wave height observations in high resolution numerical wave models is studied and evaluated. In particular, altimeter satellite data provided by the European Space Agency (ESA-ENVISAT) are assimilated in the wave model WAM which operates in two different wave climate areas: the Mediterranean Sea and the Indian Ocean. The first is a wind-sea dominated area while in the second, swell is the principal part of the sea state, a fact that seriously affects the performance of the assimilation scheme. A detailed study of the different impact is presented and the resulting forecasts are evaluated against available buoy and satellite observations. The corresponding results show a considerable improvement in wave forecasting for the Indian Ocean while in the Mediterranean Sea the assimilation impact is restricted to isolated areas.

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