Observational constraints on the kinetics of the ClO-BrO and ClO-ClO ozone loss cycles in the Arctic winter stratosphere

Author:

Butz A.12,Bösch H.1,Camy-Peyret C.2,Dorf M.1,Engel A.3,Payan S.2,Pfeilsticker K.1

Affiliation:

1. Institut für Umweltphysik; University of Heidelberg; Heidelberg Germany

2. Laboratoire de Physique Moléculaire pour l'Atmosphère et l'Astrophysique; Université Pierre et Marie Curie; Paris France

3. Institut für Atmosphäre und Umwelt; J. W. Goethe University of Frankfurt; Frankfurt Germany

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference22 articles.

1. Ultraviolet absorption cross section of Cl2O2 between 210 nm and 410 nm;Burkholder;J. Phys. Chem.,1990

2. Inter-comparison of stratospheric O3 and NO2 abundances retrieved from balloon-borne direct sun observations and Envisat/SCIAMACHY limb measurements;Butz;Atmos. Chem. Phys.,2006

3. Camy-Peyret , C. P. Jeseck T. Hawat G. Durry S. Payan G. Berube L. Rochette D. Huguenin 1995 The LPMA balloon-borne FTIR spectrometer: Remote sensing of atmospheric constituents 12th Symposium on Rocket and Balloon Programmes and Related Research Lillehammer, Norway

4. Nighttime OClO in the winter arctic vortex;Canty;J. Geophys. Res.,2005

5. Multiannual simulations with a three-dimensional chemical transport model;Chipperfield;J. Geophys. Res.,1999

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