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Recovery of the tropical lower stratospheric ozone layer

✍ Scribed by Rosenfield, Joan E.; Schoeberl, Mark R.

Book ID
119666563
Publisher
American Geophysical Union
Year
2005
Tongue
English
Weight
131 KB
Volume
32
Category
Article
ISSN
1944-8007

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The distribution of many chemical constituents of the atmosphere (e.g., ozone) is at least partially determined by the distribution of net radiative heating in the atmosphere. In this paper, we demonstrate the significant effect of high cirrus clouds on the net radiative heating of the tropical lowe