Debra Weisenstein (PI)
Atmospheric and Environmental Research Inc.
dweisens@aer.com
Use of GMI Model to Study Tropospheric and Stratospheric Bromine Budgets
This proposal seeks funding for a three year research effort as part
of the GMI Science Team under the NASA Modeling, Analysis and Prediction
program. The GMI model will be used as a tool to investigate the
importance of short-lived bromine compounds to tropospheric and stratospheric
chemistry, including trends in column ozone. Measurements of stratospheric
BrO imply nonzero concentrations of Bry at the tropopause, a result not
obtained with models which include only CH3Br and the halons. A
recent study by Salawitch et al. has shown that lower stratospheric ozone
loss would be significantly increased by assuming an additional 4-8 pptv
of Bry at the tropopause and throughout the stratosphere, especially
during times of aerosol enhancement following volcanic eruptions. Short-lived
organic bromine compounds of biogenic origin are likely to account for
the excess Bry. We propose to use the GMI model to investigate
the budget of Bry by modeling short-lived organic bromine compounds,
including CHBr3, CH2Br2, CH2BrCl, CHBr2Cl, CHBrCl2, and C2H4Br2. We
will develop emission inventories of each gas and examine the resulting
distributions of each compound individually. We will then examine
the distribution of Bry from all bromine compounds. Comparison
of modeled BrO with observations from GOME, SCIAMACHY, and in situ instruments
will help us to quantify the bromine budget in both troposphere and stratosphere. Observed
seasonal, latitudinal, and interannual variability in BrO will help in
validating sources. Knowledge of the sources and budgets of total bromine
will be necessary to the prediction of future trends in ozone and other
trace gases, as the sources of these biogenic compounds may vary with
sea surface temperature and ocean productivity, leading to climatic feedbacks.
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