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Dehydration potential of ultrathin clouds at the tropical tropopause
Author(s) -
Luo B. P.,
Peter T.,
Fueglistaler S.,
Wernli H.,
Wirth M.,
Kiemle C.,
Flentje H.,
Yushkov V. A.,
Khattatov V.,
Rudakov V.,
Thomas A.,
Borrmann S.,
Toci G.,
Mazzinghi P.,
Beuermann J.,
Schiller C.,
Cairo F.,
Di Donfrancesco G.,
Adriani A.,
Volk C. M.,
Strom J.,
Noone K.,
Mitev V.,
MacKenzie R. A.,
Carslaw K. S.,
Trautmann T.,
Santacesaria V.,
Stefanutti L.
Publication year - 2003
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2002gl016737
Subject(s) - cirrus , tropopause , atmospheric sciences , stratosphere , troposphere , ice cloud , altitude (triangle) , environmental science , radius , particle (ecology) , ice nucleus , adiabatic process , climatology , physics , geology , radiative transfer , optics , thermodynamics , oceanography , geometry , mathematics , computer security , computer science , nucleation
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.