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Which consequence results on polar jet streams due to thermal expansion?

A)Weaker zonal wind intensity equatorward
B)Steeper isobaric surface height gradient
C)Enhanced Rossby wave formation instability
D)Decreased meridional temperature contrast poleward

💡 Explanation

Enhanced warming at high latitudes from thermal expansion reduces the meridional temperature gradient; because baroclinic instability is proportional to the temperature gradient, Rossby wave amplitude increases, therefore the increased Rossby waves, rather than stable zonal flow, causes jet stream meandering.

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