The impact of stratospheric aerosol heating on the frozen hydrometeor transport pathways in the tropical tropopause layer

The exceptionally low temperature in the tropical tropopause layer (TTL) restricts the amount of water vapor entering the stratosphere. However, moisture may also enter the stratosphere in its frozen state, and the amount thereof depends on hydrometeor sedimentation and air vertical velocity. We inv...

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Detalles Bibliográficos

Autores principales:	C A Kroll, S Fueglistaler, H Schmidt, T Dauhut, C Timmreck
Formato:	Artigo
Lenguaje:	Inglês
Publicado:	IOP Publishing 2024-01-01
Colección:	Environmental Research Letters
Materias:	stratospheric moisture budget deep convection heating perturbation tropical tropopause layer volcano geoengineering
Acceso en línea:	https://doi.org/10.1088/1748-9326/ad33d0
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