Longpath DOAS observations of surface BrO at Summit, Greenland

Abstract. Reactive halogens, and in particular bromine oxide (BrO), have frequently been observed in regions with large halide reservoirs, for example during bromine catalyzed coastal polar ozone depletion events. Much less is known about the presence and impact of reactive halogens in areas without...

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Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Stutz, J., Thomas, J. L, Hurlock, S. C, Schneider, M., von Glasow, R., Piot, M., Gorham, K., Burkhart, J. F, Ziemba, L., Dibb, J. E, Lefer, B. L
Format: Article in Journal/Newspaper
Language:English
Published: eScholarship, University of California 2011
Subjects:
Physical Sciences and Mathematics
absorption cross-sections
boundary-layer
ozone destruction
tropospheric bro
peroxy-radicals
chemistry
temperature
region
snow
air
Greenland
Online Access:http://www.escholarship.org/uc/item/38f4d6sr
Description
Summary:Abstract. Reactive halogens, and in particular bromine oxide (BrO), have frequently been observed in regions with large halide reservoirs, for example during bromine catalyzed coastal polar ozone depletion events. Much less is known about the presence and impact of reactive halogens in areas without obvious halide reservoirs, such as the polar ice sheets or continental snow.

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