New observations of a large concentration of ClO in the springtime lower stratosphere over Antarctica and its implications for ozone-depleting chemistry-Reference-Cited by-同舟云学术

New observations of a large concentration of ClO in the springtime lower stratosphere over Antarctica and its implications for ozone-depleting chemistry

Published:1989 Issue:D9 Volume:94 Page:11423
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

de Zafra R. L.,Jaramillo M.,Barrett J.,Emmons L. K.,Solomon P. M.,Parrish A.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jd/v094/iD09/JD094iD09p11423/JD094iD09p11423.pdf

Reference20 articles.

1. The close relationship between Antarctic total-ozone depletion and cooling of the antarctic low stratosphere;Angel;Geophys. Res. Lett.,1986

2. Formation of the Antarctic ozone hole by the ClO dimer mechanism;Barrett;Nature,1988

3. In situ observations of ClO in the Antarctic: ER-2 aircraft results from 54deg; to 72°S latitude;Brune;J. Geophys. Res.,1989

4. Inverse problem in radiative transfer: Determination of atmospheric parameters;Chahine;J. Atmos. Sci.,1970

5. On the cooling of stratospheric temperature at Syowa, Antarctica;Chubachi;Geophys. Res. Lett.,1986

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