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Published byYuliani Kurniawan Modified over 6 years ago
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Evaluating Lower Tropospheric Ozone Simulations Using GOME/SCIAMACHY/OMI Observations of NO2 and HCHO Randall Martin Aaron Van Donkelaar Chris Sioris Kelly Chance Arlene Fiore
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SCIAMACHY Tropospheric NO2 Columns
May-July 2004
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Tropospheric NO2 Columns Evaluate NOx Emissions
SCIAMACHY NO2 (1015 molec cm-2) May-July 2004 GEOS-CHEM NO2 (1015 molec cm-2)
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Significant Model/Measurement Differences Exist
SCIAMACHY NO2 (1015 molec cm-2) May-July 2004 SCIA – GEOS-CHEM (1015 molec cm-2)
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Errors in the NO2 and HCHO Retrievals from Aerosols, Clouds, Surface Reflectivity Largely Cancel in their Ratio Solar Io Backscattered intensity IB Scattering by Earth surface and by atmosphere
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HCHO/NO2 Column Ratio Consistent with Model Overestimate of NOx Emissions from Biomass Burning
GOME GEOS-CHEM JULY 1997 Tropospheric HCHO/NO2 Column Ratio
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HCHO/NO2 Ratio is Also An Interesting Indicator
HCHO/NOy Ratio Used as Indicator Would like to Observe from Space… (ppbv) NOx-Saturated NOx-Sensitive Sillman and He, 2002
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Conduct Three Simulations With GEOS-CHEM CTM to Diagnose Quality of HCHO/NO2 Column Indicator
Base Case Reduce Anthropogenic NOx Emissions by 50% Reduce Anthropogenic VOC Emissions by 50%
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Tropospheric HCHO/NO2 Column Ratio Is an Indicator of the Sensitivity of Afternoon Surface Ozone to NOx and VOC Emissions GEOS-CHEM Model Calculation For Polluted Regions, Mar-Nov NOx Saturated NOx Sensitive
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NOx-Sensitive Conditions Over Most Polluted Regions During August Major Industrial Areas are Clear Exceptions GOME GEOS-CHEM
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Seasonal Progression from NOx-Sensitive to NOx-Saturated Conditions
GEOS-CHEM GOME More Frequent Ozone Episodes in Fall
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