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Which reversal above the tropopause weakens the westerlies?

  • A.The Coriolis parameter changes sign as the flow crosses from one hemisphere into the other one
  • B.The pressure gradient vanishes
  • C.The stratification becomes so strong that the geostrophic relation ceases to be valid at that level
  • D.The horizontal temperature gradient changes sign

Answer: D

In the lower stratosphere the polar region is warmer than the tropics, because the tropical tropopause is much higher and therefore much colder, so the thermal wind reverses to easterly. Integrating that reversed shear upward reduces the westerly wind above the jet core. The Coriolis parameter does not change sign within a hemisphere, and the geostrophic relation remains perfectly valid in the stratosphere.

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