1

In middle latitudes (say near 45°; see Table 6.1), f ~ 2Q/V2 = 1.03 x 10-4s-1. So given our typical numbers, Ro ~ 0.1 and we see that the Rossby number in the atmosphere is small. We will find in Section 9.3 that Ro ~ 10-3 for large-scale ocean circulation.

The smallness of Ro for large-scale motion in the free atmosphere and ocean4 implies that the acceleration term in Eq. 6-43 dominates the Coriolis term, leaving

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