A PHOTOCHEMICAL MODEL FOR THE SPACE-TIME VARIATIONS OF THE OXYGEN ALLOTROPES IN THE 20 TO 100 KM LAYER,
STOCKHOLM UNIV (SWEDEN) INTERNATIONAL METEOROLOGICAL INST
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A time dependent model atmosphere is developed which will provide the height distribution of ozone as a function of location, time of year, time of day and meteorological conditions in the absence of transport and diffusion. The resulting distributions are then compared to the photochemical equilibrium distribution as obtained from the infinite-day approximations, i.e. those stationary solutions obtained by assuming that time goes to infinite with the radiation remaining constant.