MODEL SENSITIVITY TO SPACE- AND IN SITU- BASED SUB-GRID FLUX PARAMETERIZATION

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium MODEL SENSITIVITY TO SPACE- AND IN SITU- BASED SUB-GRID FLUX PARAMETERIZATION Gad Levy NorthWest Research Associates and Jordan C. Alpert NCEP/Environmental Modeling Center http://www.nwra.com/resumes/levy/ papers/ January 13,2005: 85thAMS Meeting

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MODEL SENSITIVITY TO SPACE- AND IN SITU- BASED SUB-GRID FLUX PARAMETERIZATION. Gad Levy NorthWest Research Associates and Jordan C. Alpert NCEP/Environmental Modeling Center http://www.nwra.com/resumes/levy/papers/ January 13,2005: 85thAMS Meeting. Motivation & Background. - PowerPoint PPT Presentation

Transcript of MODEL SENSITIVITY TO SPACE- AND IN SITU- BASED SUB-GRID FLUX PARAMETERIZATION

Page 1: MODEL SENSITIVITY TO SPACE- AND IN SITU- BASED SUB-GRID FLUX PARAMETERIZATION

10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

MODEL SENSITIVITY TO SPACE- AND IN SITU- BASED SUB-GRID FLUX PARAMETERIZATION

Gad LevyNorthWest Research Associates

andJordan C. Alpert

NCEP/Environmental Modeling Center

http://www.nwra.com/resumes/levy/papers/

January 13,2005: 85thAMS Meeting

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Motivation & Background

o Significant uncertainty in model fluxes due to unresolved subgrid variability.

o Some variability is consistent and can be parameterized based on observations.

o Large-scale atmospheric models surface fluxes are sensitive to unresolved (subgrid) variability in the wind (bulk formulas: function of the surface winds).

o Advances in observing systems allow parameterizing subgrid flux due to wind directional variability.

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Objective and Method

o Test the impact of a subgrid parameterization (Levy and Vickers, 1999 and Levy, 2000) on the NCEP operational forecasting model.

Sensitivity tests:o Controlo Parameterization applied

with land mask (ASF1)o Parameterization applied

globally (ASF2)

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

The Parameterization1

o Accounts for subgrid variability due to directional variability.

o Formulated as a velocity scale term added to current model bulk formulation.

o Formulated as a function of model grid scale.

o Based on a best fit of collocated scatterometers (2) and buoy data.

1Levy & Vickers, 1999; Levy, 2000

Fφ = ρ ⋅Cφ ⋅V(Φ sfc − Φ)

U = (V2 + Vsg2)1/2

Vsg =(X/D-1)

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

The Parameterization (cont’d)

o Some seasonal and regional variability is evident in data used

o Flux enhancement) is largest for low winds & for larger grids.

o Satellite (ERS, NSCAT, Qscat) /buoy results consistent with aircraft results (including over land and equatorial)

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Effect of Parameterization on Fluxes

Estimated based on climatology, Quickscat, and assumed 250 km grid

Latent Heat Sensible Heat Momentum

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Model; Experimental Design; Limitations

o NCEP global forecasts system (GFS) model used

o Spectral model using a 64 level sigma vertical coordinate system

o Triangular truncation of T254 with a physical Gaussian grid of 768x384

o Existing model flux parameterization already include stratification effects; low-wind minimum

o Model run globally

o Mean values for Vsg used (regional variation neglected)

o Vsg likely underestimated over land

o Only one case (5 days forecast with initial conditions from 8 February 2004 ) run

o Impact of momentum flux enhancement hard to assess in non-coupled model

o Focus on W. Hemisphere

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

The Synoptic Scenario (1000 mb)

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Latent Heat Flux Evolution (ASF2)

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Precipitation Systems Evolution

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Impact on Heat Fluxes

o All significant impacts limited to just a few locationso Significant (20%-80%) impact in LHF in convective (tropical)

systems shows early; reflected in convective precipitationo Impact in LHF at mid/high latitudes shows later; limited to frontal

systems; reflected in geopotential and (total) precipitation redistribution

o Significant impact in sensible heat flux limited (frontal & land)

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Impact on precipitation

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10.1 Levy & Alpert: Model sensitivity to sub-grid flux parameterization- 9th IOAS-AOLS Symposium

Summary and Conclusionso Parameterization has significant direct (flux

enhancement) and indirect (convective and total precipitation, synoptic wave amplification) impacts on GFS forecasts

o Significant impacts are not evenly distributedo Impacts on middle and higher latitude systems:

• amplify the synoptic waves and change their propagation• redistribute stratiform and convective precipitation• impacts develop (noted) later (at 96 hrs. or 120 hrs.)

o Impacts on equatorial and tropical systems:• enhance latent heat fluxes • enhance tropical convective precipitation• Impacts develop early (at 24 hrs.)