Ozone loss in middle latitudes and the role of the Arctic polar vortex
- 15 August 1995
- journal article
- Published by The Royal Society in Philosophical Transactions A
- Vol. 352 (1699) , 241-245
- https://doi.org/10.1098/rsta.1995.0067
Abstract
There have been a number of different suggestions as to the cause of the observed ozone decline over middle latitudes. Here, the particular impact of polar processes on the middle latitude lower stratosphere is discussed. Recent studies suggest that air, recently activated and then torn from the edge of the polar vortex, contributes to the observed ozone decrease. For example, observational and modelling studies both indicate that there is an important role for filaments of vortex air being stripped away from the vortex edge. However, there appears to be little support for the idea of the vortex as a massive ‘flowing processor’ through which large quantities of air, primed for ozone destruction, are transported.Keywords
This publication has 7 references indexed in Scilit:
- Early modelling results from the SESAME and ASHOE campaignsFaraday Discussions, 1995
- A 3D transport model study of chlorine activation during EASOEGeophysical Research Letters, 1994
- Some case studies of chlorine activation during the EASOE CampaignGeophysical Research Letters, 1994
- A three-dimensional model comparison of PSC processing during the Arctic winters of 1991/1992 and 1992/1993Annales Geophysicae, 1994
- Breaking Rossby Waves in a Model Stratosphere Diagnosed by a Vortex-Following Coordinate System and a Technique for Advecting Material ContoursJournal of the Atmospheric Sciences, 1994
- Rapid descent of mesospheric air into the stratospheric polar vortexGeophysical Research Letters, 1993
- Tracer exchange between tropics and middle latitudesGeophysical Research Letters, 1992