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- W1610137 abstract "We present an overview of the processes leading to the ozone hole in the lower stratosphere with an emphasis on the role of transport and mixing. It is shown that the polar vortex behaves as a chemical container owing to the existence of a barrier to transport along its edge, only broken by sparse filamentary structures. Mixing is governed by chaotic layer wise motion down to horizontal scale of about 10 km. Difficulties in modelling non diffusive mixing may lead to serious underestimates of the ozone depletion." @default.
- W1610137 created "2016-06-24" @default.
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- W1610137 date "1999-01-01" @default.
- W1610137 modified "2023-09-25" @default.
- W1610137 title "The Ozone Hole" @default.
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- W1610137 doi "https://doi.org/10.1007/978-1-4615-4697-9_10" @default.
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