A general circulation model simulation of the springtime Antarctic ozone decrease and its impact on mid‐latitudes
- 20 February 1990
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Solid Earth
- Vol. 95 (D2), 1883-1898
- https://doi.org/10.1029/jd095id02p01883
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- In situ observations of ClO in the Antarctic: ER‐2 aircraft results from 54°S to 72°S latitudeJournal of Geophysical Research: Solid Earth, 1989
- Kinetics of O3 destruction by ClO and BrO within the Antarctic vortex: An analysis based on in situ ER‐2 dataJournal of Geophysical Research: Solid Earth, 1989
- Mountain waves, polar stratospheric clouds, and the ozone depletion over AntarcticaJournal of Geophysical Research: Solid Earth, 1989
- Formation of the Antarctic ozone hole by the CIO dimer mechanismNature, 1988
- Two‐dimensional modelling of the Antarctic lower stratosphereGeophysical Research Letters, 1988
- The stability and photochemistry of dimers of the ClO radical and implications for Antarctic ozone depletionNature, 1988
- A GCM simulation of the ozone seasonal variations at high latitudes in the Southern HemisphereGeophysical Research Letters, 1986
- Southern hemisphere medium‐scale waves and total ozone disturbances in a spectral general circulation modelJournal of Geophysical Research: Solid Earth, 1986
- A Simple Parameterization of the Large-Scale Effects of Cumulus ConvectionMonthly Weather Review, 1985
- Wind stress on a water surfaceQuarterly Journal of the Royal Meteorological Society, 1955