List of Figures:
|
Figure 1.(a), ( b) and (c ): Horizontal decoupling test in clear sky condition. This test shows the sensitivity of 2m temperature (b) and relative humidity (c) to a well known initial perturbation box of mean soil moisture content Wp (a). |
Figure 2.(a), (
b) and (c
): Same as Figure 1 for a box placed near to the north-eastern side of the
domain (meteorological perturbed conditions). |
(a) |
(a) |
(b) |
(b) |
(c) |
(c) |
Figure 3. Evaluation of the mean soil moisture perturbation
strategy. K matrix for T2m (Wp correction) for given perturbations:
(a) coherent, (b
) coherent (average of 10 members), (c
) conditional, (d) chess-type (1
member) and (e) chess-type (2 members).
(a) |
(b) |
|
|
(c) |
(d) |
(e) |
Figure 4. (a) Evaluation of OI coefficient for T2m (Wp correction) and (b ) equivalent 2d-var gain matrix.
|
(b) |
Figure 5.: K matrix for 2000/06/16 12 UTC as result of
chess-type perturbation (2 members) and Laplacian smoothing.
(a) K value for T2m (Wp correction), (
b) K value for RH2m (Wp correction).
(a) |
(b) |
Figure 6.: Soil Wetness Index for 2000/06/16 12 UTC ( ARPEGE/ALADIN oper.).
|
