Recent Changes Implemented into the Global Forecast System at NMC

M. Kanamitsu National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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J.C. Alpert National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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K.A. Campana National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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P.M. Caplan National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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D.G. Deaven National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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M. Iredell National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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B. Katz National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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H.-L. Pan National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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J. Sela National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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G.H. White National Meteorological Center, Development Division, Global Weather and Climate Modeling Branch

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Abstract

A number of improvements were implemented on 6 March 1991 into the National Meteorological Center's global model, which is used in the global data assimilation system (GDAS), the aviation (AVN) forecast, and the medium-range forecast (MRF):

  • The horizontal resolution of the forecast model was increased from triangular truncation T80 to T126, which corresponds to an equivalent increase in grid resolution from 160 km to 105 km.

  • The use of enhanced orography has been discontinued and replaced by mean orography.

  • A new marine-stratus parameterization was introduced.

  • A new mass-conservation constraint was implemented.

  • The horizontal diffusion in the medium scales was reduced by adopting the Leith formulation.

  • A new, more accurate sea-surface temperature analysis is now used.

In this note, we discuss each of the changes and briefly review the new model performance.

Abstract

A number of improvements were implemented on 6 March 1991 into the National Meteorological Center's global model, which is used in the global data assimilation system (GDAS), the aviation (AVN) forecast, and the medium-range forecast (MRF):

  • The horizontal resolution of the forecast model was increased from triangular truncation T80 to T126, which corresponds to an equivalent increase in grid resolution from 160 km to 105 km.

  • The use of enhanced orography has been discontinued and replaced by mean orography.

  • A new marine-stratus parameterization was introduced.

  • A new mass-conservation constraint was implemented.

  • The horizontal diffusion in the medium scales was reduced by adopting the Leith formulation.

  • A new, more accurate sea-surface temperature analysis is now used.

In this note, we discuss each of the changes and briefly review the new model performance.

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