WS Test program results for streamfunction

Ross Bannister, September 2004
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4.1 The results (MetO and WS)

Experiment C: Covariance diagnostics for streamfunction found from the MetO scheme'

Fig C.1: Latitude/height variances (MetO) Fig C.2: Wavenumber/height correlations with level 21 (about 500 hPa) (MetO)

Experiment E: Covariance diagnostics for streamfunction found from the WS scheme, 4 bands (optimal) top-hat T-transform, triangular U-transform'

Fig E.1: Latitude/height variances (MetO) Fig E.2: Wavenumber/height correlations with level 21 (about 500 hPa) (WS)

Experiment G: Covariance diagnostics for streamfunction found from the WS scheme, 4 bands (optimal) top-hat T-transform, top-hat U-transform'

Fig G.1: Latitude/height variances (MetO) Fig G.2: Wavenumber/height correlations with level 21 (about 500 hPa) (WS)

Experiment I: Covariance diagnostics for streamfunction found from the WS scheme, 4 bands (optimal) triangular T-transform, triangular U-transform'

Fig I.1: Latitude/height variances (MetO) Fig I.2: Wavenumber/height correlations with level 21 (about 500 hPa) (WS)

Experiment K: Covariance diagnostics for streamfunction found from the WS scheme, 1 band (optimal) top-hat T-transform, triangular U-transform'

Fig K.1: Latitude/height variances (MetO) Fig K.2: Wavenumber/height correlations with level 21 (about 500 hPa) (WS)

Experiment M: Covariance diagnostics for streamfunction found from the WS scheme, 10 bands (optimal) top-hat T-transform, triangular U-transform'

Fig M.1: Latitude/height variances (MetO) Fig M.2: Wavenumber/height correlations with level 21 (about 500 hPa) (WS)