Geophysical Research Letters · 2003 · 85 citations · 23 references
Natural SciencesEarth SciencesMeteorologyAtmospheric ScienceCloud PhysicsTropical MeteorologyCloud DynamicsCloud PropertiesCryosphere ClimatologyTropical Atmospheric DynamicsTropical Boundary LayerAdiabatic CoolingDehydration BehaviorDehydration StabilityIce-phase MicrophysicsOsmotic DehydrationTotal Water ContentTropopause DynamicsTroposphere Structure
We report on the first simultaneous in situ and remote measurements of subvisible cirrus in the uppermost tropical troposphere. The observed cirrus, called UTTCs (ultrathin tropical tropopause clouds), are the geometrically (200–300 m) and optically (τ ≈ 10 −4 ) thinnest large‐scale clouds ever sampled (≈10 5 km 2 ). UTTCs consist of only a few ice particles per liter with mean radius ≈5 μm, containing only 1–5 % of the total water. Yet, brief adiabatic cooling events only 1–2 K below mean ambient temperature destabilize UTTCs, leading to large sedimenting particles ( r ≈ 25 μm). Due to their extreme altitude above 17 km and low particle number density, UTTCs may efficiently dehydrate air during its last encounter with the ice phase before entering the stratosphere.
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Reginald E. Newell, Sharon Gould-Stewart · Journal of the Atmospheric Sciences · 1981 · 387 citations
A dehydration mechanism for the stratosphere
Edwin F. Danielsen · Geophysical Research Letters · 1982 · 267 citations