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Global Simulation of CH3Cl
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Model Description GEOS-CHEM global 3D model (v.5.02)
DAO GEOS-STRAT with simulation year from September August 1997 Resolution: 4 º latitude x 5 º longitude, 26 layers
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CH3Cl Emissions used in this study
Sources Gg/year Data description Biogenic 2,430 Hypothetical tropical source (Lee-Taylor et al. [2001]) Biomass burning 910 GEIA Inventory (Lobert et al. [1999]) Ocean (net) 660 GEIA Inventory (Khalil et al. [1999]) 160 Calculated using saturation anomaly and transfer velocity (Khalil et al. [1999] and Wanninkhof [1992]) Salt marshes 170 Rhew et al. [1999] Anthropogenic 162 GEIA Inventory (McCulloch et al. [1999]) Wetlands 48 Varner et al. [1999]
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Emission distributions for northern and southern hemisphere
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Annual net oceanic flux
Calculated GEIA Inventory
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I-a) Concentration comparison between observations and model at six surface stations (1/2)
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I-a) Concentration comparison between observations and model at six surface stations (2/2)
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II) Vertical profile comparison between observations and model
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II) Vertical profile comparison: observations VS. model (1/7)
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II) Vertical profile comparison: observations VS. model (2/7)
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II) Vertical profile comparison: observations VS. model (3/7)
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II) Vertical profile comparison: observations VS. model (4/7)
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II) Vertical profile comparison: observations VS. model (5/7)
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II) Vertical profile comparison: observations VS. model (6/7)
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II) Vertical profile comparison: observations VS. model (7/7)
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II) Vertical profile comparison between observations and model
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III-a) Latitude-altitude concentration distributions: observations VS
III-a) Latitude-altitude concentration distributions: observations VS. model for TRACE-P region (east)
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III-a) Latitude-altitude concentration distributions: observations VS
III-a) Latitude-altitude concentration distributions: observations VS. model for TRACE-P region (east)
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III-a) Latitude-altitude concentration distributions: comparisons of biomass burning and biogenic CH3Cl to background concentrations for TRACE-P region (east)
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IV-a) Correlation CH3OH VS. CH3Cl for TRACE-P (east)
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III-b) Latitude-altitude concentration distributions: observations VS
III-b) Latitude-altitude concentration distributions: observations VS. model for TRACE-P region (west)
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III-b) Latitude-altitude concentration distributions: observations VS
III-b) Latitude-altitude concentration distributions: observations VS. model for TRACE-P region (west)
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III-b) Latitude-altitude concentration distributions: comparisons of biomass burning and biogenic CH3Cl to background concentrations for TRACE-P region (west)
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Global Simulation of CH2O
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GOME SEP 1996 GEOS-CHME SEP 1997 GEOS-CHEM (inactive OH) without Biogenic emissions
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STD Inactive OH Inact. OH w/o 3-body rxn NO NO2 PRPE
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Regional Simulations
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RCTM GEOS-CHEM MM5 data assimilation at 70x70km, 20 layers (up to 14 km), and 5 min time step output Grell scheme with mid-level downdraft Lightning NOx parameterization by Allen et al. [2000] and Pickering et al. [1998] The same chemical module as GEOS-CHEM DAO data assimilation (GEOS-3) at 4°x5°, 48 layers (to 80 km), and 6-hour time step output Full O3-NOx-HC chemistry with 24 tracers and 120 species [Bey et al., 2001] Provides initial and boundary trace gas conditions for RCTM
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500 mb
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