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Comparison of ClO data with model results: Comparison RAM chlorine monoxide and SLIMCAT-model:
Cyan: SLIMCAT model calculations on the 475 K ientropic level. Red: Peak mixing ratio of the lower ClO
peak of mm-wave measurements. It is evident, that the model can not reproduce the enhanced ClO values
after the middle of March.
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Comparison of ozone data with model results: Comparison RAM ozone and SLIMCAT-model: MM-wave
data on the 475 K insentropic level compared to calculations of a 3-d global circulation model. It is evident
that the model is not able to reproduce the chemically induced ozone loss correctly. Short period dynamical
effects are captured quite well.
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O3-loss rates: Soid line: Ozone change due to vortex averaged diabatic descent.
Full circles: Observed ozone change averaged over 20 days. Open diamonts:
Estimated chemical ozone loss rate.
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Ozone on isentropic levels: Ozone mixing ratio on levels of constant potential temperatures
(425 K » 18 km, 475 K » 20 km and 550 K » 25 km). Red:1997, blue: 1998. Changes the ozone mixing ratios
over time are a superposition of diabatic descent and chemically induced ozone depletion.
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