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arctic vortex and the latitudinal variation of tropical cirrus for the years 2004 and 2005. Explosive volcanic eruptions emit sulfur species into the stratosphere, mainly in the form of SO2. These sulfur spe-cies react with OH and H2O to form H2SO4 on a timescale less, the absorption/scattering effi...

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Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Aerosols
PSCs
Cirrus clouds
Remote sensing
Antarctic
Arctic
The Antarctic
Antarc*
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.1442
http://bernath.uwaterloo.ca/media/407.pdf
Description
Summary:arctic vortex and the latitudinal variation of tropical cirrus for the years 2004 and 2005. Explosive volcanic eruptions emit sulfur species into the stratosphere, mainly in the form of SO2. These sulfur spe-cies react with OH and H2O to form H2SO4 on a timescale less, the absorption/scattering efficiency of aerosols is such that they still show their imprint in a wide range of optical measurements. Polar stratospheric clouds are of fundamental impor-tance for the formation of the Antarctic ozone hole (Far-man et al., 1985) that occurs every year since the early

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