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The test of application of WAM model for the wind wave forecasting of the Baltic Sea

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The following presents a test of implementation of WAM- a third generation wind wave model for oceans, for computations of wave conditions on the Baltic Sea. This work presents an actual state of implementations of this model for existing in the Maritime Institute data base for bathymetry, input meteorological forces and computation possibilities, and point sout future potential of its development and implementation for operational forecasting. Special attention was given to areas near the Polish coast, where field experiments POLRODEX were performed. The computations were made for homogenous wind fields, as well as for wind fields connected with real meteorological situations.
Słowa kluczowe
Rocznik
Strony
73--82
Opis fizyczny
Bibliogr. 18 poz., rys.
Twórcy
autor
  • Department of Operational Oceanography Maritime Institute, Gdańsk, Poland
autor
  • Department of Operational Oceanography Maritime Institute, Gdańsk, Poland
Bibliografia
  • [1] Behrens A., 1998, Wave model results for the Baltic Sea -A comparison between the second generation model HYPAS and the third generation model WAM - C4 (prepared for publication).
  • [2] Funkquist L., P. Ljungemyr, 1997, Validation of HIROMB during 1995-96. SMHI Oceanogr. no 67.
  • [3] Günther, H. at all, 1992, Implementation of a third generation ocean wave model at the European Centre for Medium Range Weather Forecasts. Technical Report No 68.
  • [4] Günther, H., S. Hasselmann, P.A.E.M Jansen, 1992, The WAM model Cycle 4.0. User Manual. DKRZ, Technical Report No 4.
  • [5] Hasselmann, S, K. Hasselmann, J.H. Allender, T.P. Barnett, 1985, Computations and parameterisations of the non-linear energy transfer in gravity wave spectrum. Part I: A new method for efficient computations of the exact non-linear transfer integral. J. Phys. Oceanogr. 15, 1378.
  • [6] Hasselmann, K., 1974, On the spectral dissipation of ocean waves due to the white capping. Bound. Layer Met. 6, 107.
  • [7] Jakubiak B., M. Kalas, 1998, Assessment of numerical wind forecast in the Polish part of the Baltic Sea during the experiment POLRODEX'97. (Prepared for publication).
  • [8] Jansen, P.A.E.M., 1989, Wave induced stress and the drag of air flow over sea waves. J. Phys. Oceanogr. 19, 745.
  • [9] Jansen, P.A.E.M., 1991, Quasi-linear theory ofwind wave generation applied to wave fore-casting . J. Phys. Oceanogr. 21, 1631.
  • [10] Kałas M., A. Staskiewicz, 1998, The possibility of implementation ofWAM model as a forecasting model for the Baltic Sea, Report Maritime Institute No. 5387. (In Polish).
  • [11] Komen, G.J., S. Hasselmann, K. Hasselmann, 1984, On the existence of a fully developed windsea spectrum. J. Phys. Oceanogr. 14, 1271.
  • [12] Naguszewski A., 1997, Adaptation of forecasting model for wind waves WAMfor the Polish coastal zone, Report Institute of Hydro-Engineering. (In Polish).
  • [13] Paszkiewicz Cz., 1988, Wind waves of the Baltic Sea, AMW, Gdynia. (In Polish).
  • [14] Paplińska B., 1997, Verification of wind wave forecasting model WAM with measuring data, Report Institute of Hydro-Engineering. (In Polish).
  • [15] Paplińska B., 1998, Analysis of wind waves near Lubiat6w and Pomeranian Bay on basis for measurements 1996197- comparison with model calculations (WAM program), Report Institute of Hydro-Engineering. (In Polish).
  • [16] Paplińska B., 1998, Case study of wave dependent drag coefficient in the Baltic Sea. Contribution to Atmospheric Physic (in pres.).
  • [17] Snyder R.L., F.W. Dobson, J.A. Eliott, R.B. Long, 1981, Array measurements of atmospheric pressure fluctuations above surface gravity waves. J. Fluid. Mech. 102, 1.
  • [18] WAMDI Group, 1988, A Third Generation Ocean Wave Prediction Model. J. Phys. Oceanogr. 18, 1775.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-4ebb6961-f105-4b2e-b427-5f4178118d43
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