Tropical deep convection and tropical tropopause - Academia Sinica
Tropical deep convection and tropical tropopause - Academia Sinica
Tropical deep convection and tropical tropopause - Academia Sinica
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• Some suggest that the <strong>tropical</strong> cross<strong>tropopause</strong><br />
transport of H2O is performed<br />
by large scale ascent (e.g., Küpper et al.,<br />
2004). But there is no observations to<br />
substantiate this claim.<br />
• If even the layer above the strong<br />
<strong>convection</strong> contains sinking motion, how<br />
can we expect rising motion in large scale?
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