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An operational Baltic Sea circulation model : Part 1. Barotropic version

Lennart Funquist

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Abstract

A vertically integrated barotropic model for the Baltic Sea is described both in dynamic and numerical 1terms. The model has been ron operationally since March 1993 on a 5 x 5 km grid and is forced by interpolated 10 m winds and surface pressure from the 50 x 50 km HIRLAM atmospheric mode!. The water volume is not conserved but depends on inflow from rivers and in- or outflow through the Belt Sea and the Öresund.

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What this paper is about

A vertically integrated barotropic model for the Baltic Sea is described both in dynamic and numerical 1terms. The model has been ron operationally since March 1993 on a 5 x 5 km grid and is forced by interpolated 10 m winds and surface pressure from the 50 x 50 km HIRLAM atmospheric mode!. The water volume is not conserved but depends on inflow from rivers and in- or outflow through the Belt Sea and the Öresund.

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Available abstract

A vertically integrated barotropic model for the Baltic Sea is described both in dynamic and numerical 1terms. The model has been ron operationally since March 1993 on a 5 x 5 km grid and is forced by interpolated 10 m winds and surface pressure from the 50 x 50 km HIRLAM atmospheric mode!. The water volume is not conserved but depends on inflow from rivers and in- or outflow through the Belt Sea and the Öresund.

Key concepts: Barotropic fluid, Circulation (fluid dynamics), Baltic sea, Climatology, Geology, General Circulation Model, Oceanography, Meteorology

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