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Which consequence results when intensified Hadley cell circulation interacts with increased Arctic warming?

A)Weakened mid-latitude temperature gradients
B)Strengthened tropical cyclone formation rates
C)Expanded subtropical desert regions
D)Accelerated thermohaline circulation slowdown

💡 Explanation

When intensified Hadley cell circulation interacts with Arctic warming, increased atmospheric stability in the subtropics arise because sinking air from a stronger Hadley cell suppresses precipitation, causing desert expansion. Therefore, expanded subtropical desert regions result, rather than temperature gradient changes or storm intensification which require different atmospheric conditions.

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