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| Titel |
Impact of large solar zenith angles on lower stratospheric dynamical and chemical processes in a coupled chemistry-climate model |
| VerfasserIn |
D. Lamago, M. Dameris, C. Schnadt, V. Eyring, C. Brühl |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1680-7316
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| Digitales Dokument |
URL |
| Erschienen |
In: Atmospheric Chemistry and Physics ; 3, no. 6 ; Nr. 3, no. 6 (2003-11-12), S.1981-1990 |
| Datensatznummer |
250001334
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| Publikation (Nr.) |
 copernicus.org/acp-3-1981-2003.pdf |
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| Zusammenfassung |
Actinic fluxes at large solar zenith angles
(SZAs) are important for atmospheric chemistry, especially under twilight conditions in polar winter and spring. The
results of a sensitivity experiment employing the fully coupled 3D chemistry-climate model
ECHAM4.L39(DLR)/CHEM have been analysed to quantify the impact of SZAs larger than
87.5º on dynamical and chemical processes in the lower stratosphere, in particular their influence on the ozone layer.
Although the actinic fluxes at SZAs larger than 87.5º are small, ozone concentrations are significantly affected because daytime photolytic
ozone destruction is switched on earlier, especially at the end of polar night the conversion of
Cl2 and Cl2O2 into ClO in the lower stratosphere. Comparing climatological mean ozone column values of a
simulation considering SZAs up to 93º with those of the sensitivity run with SZAs
confined to 87.5º total ozone is reduced by about 20% in the polar Southern Hemisphere, i.e., the ozone hole is
"deeper'' if twilight conditions are considered in the model because there is about 4 weeks more time for ozone
destruction. This causes an additional cooling of the polar lower stratosphere
(50 hPa) up to -4 K with obvious consequences for chemical processes. In the Northern Hemisphere the impact of large SZAs cannot be determined on the
basis of climatological mean values due to the pronounced dynamic variability
of the stratosphere in winter and spring. This study clearly shows the necessity
of considering large SZAs for the calculation of photolysis rates in atmospheric
models. |
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