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The role of water-vapour photodissociation on the formation of a deep minimum in mesopause ozone
A one-dimensional atmospheric photochemical model with an altitude grid of about 1.5 km was used to examine the structure of the global mean vertical ozone pro®le and its night-time-to-daytime variation in the upper atmosphere. Two distinct ozone layers are predicted, separated by a sharp drop in the ozone concentration near the mesopause. This naturally occurring mesopause ozone deep minimum is primarily produced by the rapid increase in the destruction of water vapour, and hence increase indoi:10.1007/s00585-998-0189-4 fatcat:rw2ksm77zraehfwahw4bemfgba