A high-resolution one-layer model of breaking planetary waves in the stratosphere

Details A high-resolution one-layer model of breaking planetary waves in the stratosphere A high-resolution one-layer model of breaking planetary waves in the stratosphere

Aug 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987natur.328..590j&link_type=abstract

Nature (ISSN 0028-0836), vol. 328, Aug. 13, 1987, p. 590-596. Research supported by the Meteorological Office, Nuffield Foundati

Mathematics

Logic

239

Atmospheric Models, High Resolution, Planetary Waves, Stratosphere, Atmospheric Chemistry, Barotropism, Numerical Integration, Ozone Depletion, Vorticity, Winter, Zonal Flow (Meteorology)

Scientific paper

Numerical integrations of a one-layer hemispheric model of the winter stratosphere have been carried out at very high resolution (of the order of a fraction of a degree of latitude). The numerical experiments simulate planetary-wave breaking and polar-vortex erosion under conditions far closer to the real winter stratosphere than those assumed in earlier, 'critical-layer' models. The model has implications for stratospheric photochemistry and the Antarctic ozone hole problem.

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