Indicators of transport and vertical motion from correlations between in situ measurements in the Airborne Antarctic Ozone Experiment

Author:

Murphy D. M.,Tuck A. F.,Kelly K. K.,Chan K. R.,Loewenstein M.,Podolske J. R.,Proffitt M. H.,Strahan S. E.

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

Reference35 articles.

1. Kinetics of O3 destruction by ClO and BrO within the Antarctic vortex: An analysis based on in situ ER-2 data;Anderson;J. Geophys. Res.,1989

2. Ozone destruction by chlorine radicals within the Antarctic vortex: The spatial and temporal evolution of ClO — O3 anticorrelation based on in situ ER-2 data;Anderson;J. Geophys. Res.,1989

3. Photochemical trajectory modeling in the springtime Antarctic, 2, Seasonal behavior of the ozone hole;Austin;J. Geophys. Res.,1989

4. Large-scale variations in ozone and polar stratospheric clouds measured with airborne lidar during formation of the 1987 ozone hole over Antarctica;Browell;Proceedings of the Polar Ozone Workshop,1988

5. Nitric acid cloud formation in the cold Antarctic stratosphere: A major cause for the springtime “ozone hole”;Crutzen;Nature,1986

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