The angle at which surface winds cross isobars is to a large degree dependent on the roughness of the terrain.

Name: The angle at which surface winds cross isobars is to a large degree dependent on the roughness of the terrain.
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The angle at which surface winds cross isobars is influenced by the Coriolis effect and friction, with the latter being significantly affected by the roughness of the terrain. Rougher terrain increases friction, which can alter the angle at which wind crosses isobars.

The Angle at Which Surface Winds Cross Isobars Is to a Large