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Explore O3-HOx-NOx system behavior, source contributions, GEOS-CHEM vs. observations, model comparisons, and more.
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Asian outflow and chemical evolution of ozone and nitrogen oxides over the Pacific Mathew Evans, Daniel Jacob, Harvard Group, TRACE-P Science Team et al.
Questions • How well do we understand the behavior of the O3-HOx-NOx system in Asian outflow? • What is the relative contribution of different sources on O3 and nitrogen oxides in Asian outflow over the Pacific?
GEOS CHEM vs observations Model sampled along flight tracks Outputs concentrations and rates
Comparison of model and GOME NO2 preliminary slant column K Chance, T Kurosu Smithsonian Astrophysical Observatory R.V. Martin, P.I. Palmer, Harvard
Model and observed O3 West Mid North South Model / Measurements
Model and observed NO West Mid North South Model / Measurements
Model and observed OH West Mid North South Model / Measurements
NOy to CO Anthropogenic vs Biomass burning sources North South
O3 - PAN relationshipModel versus observations (color = Latitude) High latitude Boundary layer Low latitude Free troposphere
Impact of anthro. emissionson March NOxFractional decrease in NOx when anthropogenic emissions are shut off Fractional decrease in NOx concentration
Impact of anthro. emissions on March O3 Decrease in concentration when anthropogenic emissions are shut off Difference in O3 concentration (ppbv)
O3 model / observed ensemble of TRACE-P data and sensitivity simulations
Preliminary conclusions • Distribution of NOx observed during TRACEP is consistent with our understanding of combustion sources • Large O3 anthropogenic enhancement in boundary layer Asian outflow with destruction during aging over Pacific. • Free tropospheric O3 in Asian outflow has comparable sources from anthropogenic, biomass burning and lightning • Large model overestimate of HOx and H2O2 and CH2O??? • Mystery VOC source over Hainan???