The UK Meteorological Office Operational Wave Model (BMO)
The operational wave prediction model used by the UK Meteorological Office has a grid point representation of the wave field. This is usually defined on a polar stereographic projection of the earth’s surface, and it can be initialized with any grid length and any shape or size of ocean basin, subject to core storage constraints. It has a general nesting capability, permitting any model to obtain inflow boundary conditions from any other. Operationally, two models are run. One covers much of the Northern Hemisphere, with a grid length at 60°N of 300 km. This provides boundary conditions for a 50-km-grid-length model of the Northwest European Continental Shelf. An extended description of the model is given in Golding (1983).
KeywordsBeach Advection Refraction sinO
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- Bretschneider, C. L. (1954): Generation of wind waves over a shallow bottom. Technical Memorandum 51, Corps of Engineers Beach Erosion Board, Department of the Army, Washington, D.C.Google Scholar
- Findlater, J., T. N. S. Harrower, G. A. Howkins, and H. L. Wright (1966): Surface and 900 mb wind relationships. Meteorological Office Science Paper 23, HMSO, London.Google Scholar
- Golding, B. W. (1977): A depth dependent wave model for operational forecasting. Turbulent Fluxes through the Sea Surface, Wave Dynamics, and Prediction (A. Favre and K. Hasselmann, eds.), Plenum Press, New York. 593–604.Google Scholar