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Geography

Which consequence results when strong pressure gradients interact with the Coriolis effect in the upper troposphere?

A)Formation of geostrophic winds
B)Development of thermal inversions
C)Intensification of Hadley cells
D)Creation of katabatic winds

💡 Explanation

When a pressure gradient exists, air moves from high to low pressure, but the Coriolis effect deflects this movement depending on hemisphere creating a curved path. Therefore geostrophic winds are formed, rather than inversions, Hadley cell intensification, or katabatic winds which involve different thermal and topographical mechanisms.

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