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On the temperature dependence of polar stratospheric clouds
Author(s) -
Fiocco Giorgio,
Fuà Daniele,
Cacciani Marco,
Girolamo Paolo Di,
De Luisi John
Publication year - 1991
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 - 10.1029/90gl02585
Subject(s) - polar , atmospheric sciences , lidar , stratosphere , aerosol , environmental science , materials science , meteorology , geology , physics , remote sensing , astronomy
Polar stratospheric clouds were frequently observed by lidar at the Amundsen‐Scott South Pole Station during May–October 1988. The dependence of the bakscattering cross section on the temperature can be referred to transitions of the HNO 3 /H 2 O system: it appears possible to distinguish the pure trihydrate from the mixed ice‐trihydrate phase in the composition of the aerosol and, in some cases, to bracket the HNO 3 and H 2 O content of the ambient gas, and to provide indications on the size of the particles.

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