Examples of geostrophic

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Whereas this wave is stationary and geostrophic for infinitesimal amplitude, there is upstream propagation for finite amplitude.
Calculations were also reported on the effect of the geostrophic flow generated by the mixed-layer depth variations.
The dynamics of vertically compensated two-layer vortices (hetons) with finite cores are examined within the context of the quasi-geostrophic approximation on the f -plane.
The flow remains hydrostatic and departs from geostrophic only in the first equation of motion.
The geostrophic balance is also seen in weather maps, which show upper-level winds blowing along isobars.
This is the part of the total geostrophic pressure field which has its highs correlated with the mountain upslopes.
This differs from the energy (2.2) conserved by equations (2.1) by the replacement of the kinetic energy by its geostrophic value.
The winds then backed to 190x after 1400 hours, but remained light throughout and exhibit the expected behaviour compared to the geostrophic flow above.
A further adjustment will take place on the inertial time-scale to establish approximate geostrophic balance of the wind parallel to the ridge.
At mid-day the geostrophic flow remained westerly and of a reasonable strength.
This source represents the integral effect of the heat release by the rotation-dominated plumes at times larger than the geostrophic adjustment time.
It would be necessary to apply the method in geostrophic and isentropic coordinates, which is only practicable even in principle for a semi-geostrophic model.
Here this 'geostrophic balance' is derived, in the context of the shallow water equations, by using an approximate scale analysis.
As a result, the alongshore component of velocity is assumed to be in geostrophic balance.
Little is known about geostrophic flow over an array of obstacles representing a rough bottom.

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