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An investigation of the atmospheric sources and sinks of methyl bromide

Journal Article · · Geophysical Research Letters (American Geophysical Union); (United States)
DOI:https://doi.org/10.1029/92GL02634· OSTI ID:6711112
 [1];  [2]
  1. NASA Ames Research Center, Moffett Field, CA (United States)
  2. CNRS, Gif-sur-Yvette (France)

Methyl Bromide (CH[sub 3]Br) is a ubiquitous component of the atmosphere and has been implicated as an important player in the depletion of stratospheric ozone. Atmospheric CH[sub 3]Br abundances, interhemispheric gradients, oceanic concentrations, man-made emissions, and removal processes have been analyzed and interpreted with the help of a simple box model and a 2-D global photochemical model. Its calculated atmospheric lifetime (T) of 1.7-1.9 years, based on reaction with OH radicals, is consistent with a global source of 90-110 Gg (10[sup 9] g)/year. Consequences of a much shorter lifetime of 1.2 years, due to possible deposition/hydrolysis losses, are also considered. Available data are used to estimate a CH[sub 3]Br source that is 35% (20-50%) man-made and 65% (80-50%) natural. Oceans are substantially supersaturated and provide the most important natural source of [approx]60 (40-80) Gg/year. Within the oceans 200-300 Gg/year of CH[sub 3]Br may be produced. Indirect emissions from automobile exhaust and biomass burning can not be well quantified (1-10 Gg/year). A global trend of 0.1-0.2 ppt/year is predicted. Model results show significant vertical and seasonal variations in the atmospheric abundances and interhemispheric gradients of CH[sub 3]Br. Substantial uncertainties in calibrations, source estimates, and deposition processes are present. 12 refs., 3 figs., 2 tabs.

OSTI ID:
6711112
Journal Information:
Geophysical Research Letters (American Geophysical Union); (United States), Journal Name: Geophysical Research Letters (American Geophysical Union); (United States) Vol. 20:2; ISSN GPRLAJ; ISSN 0094-8276
Country of Publication:
United States
Language:
English