372
S. S. Karimova and M. Gade
Fig. 18.9 (continued)
forcing and the general current’s interaction with the local topography (Quadfasel
and Baudner 1993). We further note that basin-scale eddies were mainly detected
during spring season.
More quantitative information on the basin-scale eddy manifestations is summarized in Table 18.1 in chronological order. Again, we can note that only the “smallest”
two eddies were cyclonically rotating. This table also supports our finding that the
largest eddies detected in all SAR images (with diameters exceeding 120 km) used
for the present study were mainly found during spring.
S. S. Karimova and M. Gade
Fig. 18.9 (continued)
forcing and the general current’s interaction with the local topography (Quadfasel
and Baudner 1993). We further note that basin-scale eddies were mainly detected
during spring season.
More quantitative information on the basin-scale eddy manifestations is summarized in Table 18.1 in chronological order. Again, we can note that only the “smallest”
two eddies were cyclonically rotating. This table also supports our finding that the
largest eddies detected in all SAR images (with diameters exceeding 120 km) used
for the present study were mainly found during spring.