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The model column ozone is very similar to that observed by satellite. Over the Antarctic continent there are low amounts of ozone, where there has been chemical destruction. Around the edge of the vortex, between 30S and 60S, there are higher amounts of ozone. These high amounts result from the transport of ozone from the region of production in the tropics.
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© 1998.
Centre for Atmospheric Science, Cambridge University, UK.
No text or graphics can be used or reproduced without explicit written permission.
This version designed and maintained by
Dr. Glenn Carver.
Original concept and design Owen Garrett.