Oceanic bromoform emissions weighted by their ozone depletion potential

At present, anthropogenic halogens and oceanic emissions of very short-lived substances (VSLSs) both contribute to the observed stratospheric ozone depletion. Emissions of the long-lived anthropogenic halogens have been reduced and are currently declining, whereas emissions of the biogenic VSLSs are...

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Bibliographic Details
Main Authors: S. Tegtmeier, F. Ziska, I. Pisso, B. Quack, G. J. M. Velders, X. Yang, K. Krüger
Format: Article
Language:English
Published: Copernicus Publications 2015-12-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/13647/2015/acp-15-13647-2015.pdf