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geostrophic wind

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anglais
In other words, there is no vertical wind shear of the geostrophic wind.
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In the free atmosphere, geostrophic wind relationships should be used.
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This is known as a geostrophic wind.
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The geostrophic wind neglects frictional effects, which is usually a good approximation for the synoptic scale instantaneous flow in the midlatitude mid-troposphere.
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They follow the principle of geostrophic winds.
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The true wind almost always differs from the geostrophic wind due to other forces such as friction from the ground.
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In other words, no vertical wind shear of the geostrophic wind.
en.wikipedia.org
In a barotropic atmosphere, where temperature is uniform, the geostrophic wind is independent of height.
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The thermal wind is the "difference" in the geostrophic wind between two levels in the atmosphere.
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This creates a westerly geostrophic wind pattern to form in the mid-latitudes.
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