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← GeographyWhich 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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