OMI Satellite/AIRPACT-3 Comparisons
(View additional imagery: CO from AIRS instrument)
Explanation of Images
Monthly Average NO2 from OMI (Ozone Monitoring Instrument) and AIRPACT are for 1pm-2pm values only (when OMI passes over the region). Pixels with over 35% cloud cover are not included in the averaging function. An assumed GEOS-CHEM profile is used to add an estimated "below cloud" contribution to the Tropospheric Column derived from OMI.
OMI values are from the tropospheric NO2 Vertical Column Data Product from NASA. AIRPACT values are taken from mixing ratio forecasts for all vertical layers and then vertically integrated into a single Vertical Column Density value. Ratios and Residuals are also calculated and provided to give a quantitative factor & difference between the satellite observations and the modeling system.
The OMI Tropospheric NO2 algorithm assumes an annually averaged stratospheric contribution, which is subtracted from the total column measurement. Since seasonal changes in stratospheric NO2 are not factored in, a shifting bias over the whole domain can be seen. Overall, this results in OMI Tropospheric NO2 showing larger summer values and smaller winter values.
These AIRPACT results have been spatially averaged to the coarser OMI pixel resolution. Select from the monthly tabs below.
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Additional satellite products links:
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2007
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2008
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