Etudes et évaluation de processus océaniques par des hiérarchies ...
Etudes et évaluation de processus océaniques par des hiérarchies ... Etudes et évaluation de processus océaniques par des hiérarchies ...
54 CHAPITRE 4. ETUDES DE PROCESSUS OCÉANOGRAPHIQUES A. Wirth et al. / Deep-Sea Research II 49 (2002) 1279–1295 1291 tel-00545911, version 1 - 13 Dec 2010 Fig. 8. Standard deviation due to external (upper) and internal (lower) variability for the low-viscosity exps. RG-lo (contour interval is 5 m). The standard deviation due to the external part is calculated using the variance of the means over 10 realizations for each of the years 1993, 1995 and 1996. The standard deviation of the internal part is calculated using the average variance for the years 1993, 1995 and 1996.
4.1. VARIABILITY OF THE GREAT WHIRL FROM OBSERVATIONS AND MODELS55 1292 A. Wirth et al. / Deep-Sea Research II 49 (2002) 1279–1295 tel-00545911, version 1 - 13 Dec 2010 Fig. 9. As Fig. 8, but for the high-viscosity experiments RG-hi.
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54 CHAPITRE 4. ETUDES DE PROCESSUS OCÉANOGRAPHIQUES<br />
A. Wirth <strong>et</strong> al. / Deep-Sea Research II 49 (2002) 1279–1295 1291<br />
tel-00545911, version 1 - 13 Dec 2010<br />
Fig. 8. Standard <strong>de</strong>viation due to external (upper) and internal (lower) variability for the low-viscosity exps. RG-lo (contour interval is<br />
5 m). The standard <strong>de</strong>viation due to the external <strong>par</strong>t is calculated using the variance of the means over 10 realizations for each of the<br />
years 1993, 1995 and 1996. The standard <strong>de</strong>viation of the internal <strong>par</strong>t is calculated using the average variance for the years 1993, 1995<br />
and 1996.
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