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Atmospheric chemistry: Bromine explosion

Wennberg, Paul (1999) Atmospheric chemistry: Bromine explosion. Nature, 397 (6717). pp. 299-301. ISSN 0028-0836. doi:10.1038/16805. https://resolver.caltech.edu/CaltechAUTHORS:20150605-142337991

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Abstract

Bromine free radicals are emerging as important players in the photochemistry of the lower atmosphere, at least on local scales. Earlier this month, Hebestreit et al. described the discovery of air laden with bromine monoxide (BrO) wafting off the salt pans near the Dead Sea. And on page 338 of this issue, McElroy and colleagues report observations of BrO, obtained by remote measurements in the Arctic, that suggest bromine is present between the tropopause (at about 8 km height) and the top of the planetary boundary layer (~1 km). The planetary boundary layer is unlike the free troposphere that lies above it because the turbulence mixing timescale is very fast, and so exchange of gases with the surface occurs quickly (less than 1 day).


Item Type:Article
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URLURL TypeDescription
http://dx.doi.org/10.1038/16805DOIArticle
http://www.nature.com/nature/journal/v397/n6717/full/397299a0.htmlPublisherArticle
ORCID:
AuthorORCID
Wennberg, Paul0000-0002-6126-3854
Additional Information:© 1999 Macmillan Magazines Ltd.
Issue or Number:6717
DOI:10.1038/16805
Record Number:CaltechAUTHORS:20150605-142337991
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20150605-142337991
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:58061
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:05 Jun 2015 23:58
Last Modified:10 Nov 2021 21:58

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