A three-dimensional ocean-atmosphere model of the global methyl bromid
e budget is presented including an analysis of the temporally and spat
ially varying source and sink distributions. No correlation is found b
etween oceanic net biological CH,Br production, implied by surface wat
er saturation anomaly observations, and oceanic variables such as surf
ace chlorophyll and primary production; therefore model ocean fluxes a
re constrained directly by the saturation anomaly observations. The re
sulting diagnosed biological production rates imply net production in
the tropics and subtropics and net consumption at high latitudes. Resu
lts from this semicoupled ocean-atmosphere model show substantial long
itudinal variability in the atmospheric boundary layer CH,Br concentra
tions with land-ocean contrasts of 1-6 ppt due to regional industrial
and agricultural emissions on land and net fluxes into the ocean. Owin
g to an imbalance in current understanding of the global budget, our s
imulated mixing ratios of 3.5 to 6.5 ppt for the southern and northern
hemispheres, respectively, are significantly lower than available mea
surements. Sensitivity studies reducing the ocean and soil surface sin
ks slightly improve the global mean CH,Br concentration but increase t
he interhemispheric ratio further beyond that supported by observation
s. Accordingly, an apparent terrestrial missing source of 89 - 104 kT
yr(-1) is derived and applied to the model. This is of, the same order
as the sum of all other sources in the model (85 kT yr(-1)). The hemi
spheric distribution of the missing source is explored, indicating tha
t 50 - 70% of this source occurs in the southern hemisphere and is lik
ely to be biased toward tropical regions. Modeled seasonal variability
in the interhemispheric ratio at specific monitoring sites agrees wel
l with observations. The model-predicted vertical gradient of CH,Br th
rough the troposphere and lower stratosphere is also presented.