,.

Jonathan Lin1,2, Kerry Emanuel3

  • 1Lamont-Doherty Earth Observatory, Columbia University, New York, NY 10027.

概括

在热带地区,随着热带层升温,较低层平流层会变冷. 这种观察到的反相关性是由热层层对平流层施加压力的新理论解释的.

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