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The Sensitivity of Moisture Flux Partitioning in the Cold‐Point Tropopause to External Forcing

Abstract The dryness of the stratosphere is the result of air entering through the cold tropical tropopause layer (TTL). However, our understanding of the moisture flux partitioning into water vapor and frozen hydrometeors is incomplete. This raises concerns regarding the ability of General Circulat...

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Príomhchruthaitheoirí: C. A. Kroll, S. Fueglistaler, H. Schmidt, L. Kornblueh, C. Timmreck
Formáid: Artigo
Teanga:Inglês
Foilsithe / Cruthaithe: Wiley 2023-06-01
Sraith:Geophysical Research Letters
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Rochtain ar líne:https://doi.org/10.1029/2022GL102262
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