Pr. Gent et al., SCALING ANALYSIS OF CURVED FRONTS - VALIDITY OF THE BALANCE-EQUATIONSAND SEMIGEOSTROPHY, Journal of the atmospheric sciences, 51(1), 1994, pp. 160-163
Strongly curved fronts occur when the ratios of cross-front to alongfr
ont horizontal velocities and scales are comparably small for an order
one distance in the alongfront direction. This means that all three v
elocity terms in the continuity equation contribute at leading order.
The balance equations are shown to be formally accurate through two or
ders in powers of the small parameter in this situation; however, the
semigeostrophic equations are accurate only at leading order. Both app
roximate models are accurate through two orders of magnitude if the fr
ont is more weakly curved.