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geostrophic wind [ˌʤiːəʊstrɒfɪkˈwind] SUBST

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inglês
The ageostrophic wind component is the difference between actual and geostrophic wind, which is responsible for air filling up cyclones over time.
en.wikipedia.org
In the free atmosphere, geostrophic wind relationships should be used.
en.wikipedia.org
The thermal wind is the "difference" in the geostrophic wind between two levels in the atmosphere.
en.wikipedia.org
In other words, no vertical wind shear of the geostrophic wind.
en.wikipedia.org
To maintain balance, the geostrophic wind aloft and below adjust, such that regions of divergence/convergence form.
en.wikipedia.org
The geostrophic wind is directed parallel to isobars (lines of constant pressure at a given height).
en.wikipedia.org
In other words, there is no vertical wind shear of the geostrophic wind.
en.wikipedia.org
Thus, the actual wind would equal the geostrophic wind only if there were no friction and the isobars were perfectly straight.
en.wikipedia.org
This creates a westerly geostrophic wind pattern to form in the mid-latitudes.
en.wikipedia.org
The geostrophic wind neglects frictional effects, which is usually a good approximation for the synoptic scale instantaneous flow in the midlatitude mid-troposphere.
en.wikipedia.org

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