Remote sensing of NO2
3 Retrieval procedures

The task of remote sensing is to measure the concentrations of specific trace gases in the atmosphere, and particularly in the troposphere. The presence of a species in the atmosphere can be detected through the presence of characteristic absorption features in the spectrum of light passing through the atmosphere, and the concentration of the species from the amount of absorption that takes place (in accordance with the Beer-Lambert Law).

The process of data retrieval described in this section takes the earthshine spectrum measured at the satellite for each ground pixel scanned and derives a value for the concentration of NO2 in the column of troposphere above that pixel.

This section describes the procedures used to derive the concentrations of tropospheric NO2 from earthshine spectra.

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