300 Pierre De Mey and Mounir Benkiran
diffusion, vertical resolution and horizontal eddy-induced mixing in the assimilation ron.
15.3.4 Influence of horizontal and vertical resolution in the assimilation
Prior to using the 118°, 31-level model, the team had started configuring and
a)
b)
SSH allat=38N
SSH at lat=33N
Fig. 15.6 Longitude-time plots of sea-Ievel anomaly in the model: (a) at 38°N in the
Algerian Current; (b) at 33°N across the Mersa-Matruh and Shikmona systems. Unit: cm.
Contour interval: 3 cm. Negative anomalies are shaded.
testing the assimilation on a 10wer-resolution 114°, 19-1evel version of the same
model (Benkiran, 1997; Benkiran et al., 1997). The beginnings were rather frostrating because the low-resolution model did not respond in a significant manner to
diffusion, vertical resolution and horizontal eddy-induced mixing in the assimilation ron.
15.3.4 Influence of horizontal and vertical resolution in the assimilation
Prior to using the 118°, 31-level model, the team had started configuring and
a)
b)
SSH allat=38N
SSH at lat=33N
Fig. 15.6 Longitude-time plots of sea-Ievel anomaly in the model: (a) at 38°N in the
Algerian Current; (b) at 33°N across the Mersa-Matruh and Shikmona systems. Unit: cm.
Contour interval: 3 cm. Negative anomalies are shaded.
testing the assimilation on a 10wer-resolution 114°, 19-1evel version of the same
model (Benkiran, 1997; Benkiran et al., 1997). The beginnings were rather frostrating because the low-resolution model did not respond in a significant manner to