Bromine chemistry mechanism: Difference between revisions
Jump to navigation
Jump to search
No edit summary |
No edit summary |
||
Line 19: | Line 19: | ||
== Chemical Mechanism == | == Chemical Mechanism == | ||
== Chemical Lifetimes == | |||
== Source code and data files == | == Source code and data files == |
Revision as of 19:31, 1 July 2010
NOTE: Page under construction!
Overview
Bromine chemistry has been added as an option to run with SMVGEAR or KPP in v.8-03-01 as an extension to the standard model's full chemistry simulation. Important features include:
1.) Add 10 bromine tracers: Br2, Br, BrO, HOBr, HBr, BrNO2, BrONO2, CHBr3, CH2Br2, and CH3Br 2.) 4 source gases: - CH3Br: concentrations are set to average CMDL measured concentrations prior to each chemistry step. - Very short lived (VSL) source gases: - CH2Br2 and CHBr3. These account for > 80% of the VSL organic bromine through the troposphere (WMO, 2007). - Emissions are taken from Q. Liang et al. [2010] + a seasonal scaling for CHBr3 at lat > 30N described in J. Parrella et al. [in prep.] - 429 Gg CHBr3 / yr; 62 Gg CH2Br2 / yr - Sea-salt debromination: - Largely follows Yang et al. [2005], treating the debromination as an emission of Br2, constrained to measured bromide depletion factors. - 1.4 Tg Br2 / yr using the Monahan sea-salt production function and coarse aerosol bin range of 0.5 - 10 um. 3.) Wet and dry deposition for HBr, HOBr, and BrONO2.
Code should be made available soon. This wiki page is under construction, but feel free to contact Justin Parrella (parrella@fas.harvard.edu) with any questions about the code.