Rotating Fluids in Geophysics
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Paul Harry Roberts, A. M. Soward. time origin (t-,t+tQ) reproduces (13-1)» but
with a different ^ [viz. v cos tot0-K:^(sin 0)tg)/oJ ] . By suitable choice of tQ we may
eliminate the component of v parallel to k X j£ entirely. Then by (12.11)» v is ...