Abstract. Satellite measurements of atmospheric trace gases have proved to be an invaluable tool for monitoring the Earth system. When these measurements are to be used for assessing tropospheric emissions and pollution, as for example in the case of nadir measurements of nitrogen dioxide (NO₂), it is necessary to separate the stratospheric from the tropospheric signal.

The SCIAMACHY instrument offers the unique opportunity to combine its measurements in limb- and nadir-viewing geometries into a tropospheric data product, using the limb measurements of the stratospheric NO₂ abundances to correct the nadir measurements' total columns.

In this manuscript, we present a novel approach to limb/nadir matching, calculating one stratospheric NO₂ value from limb measurements for every single nadir measurement, abandoning global coverage for the sake of spatial accuracy. For comparison, modelled stratospheric NO₂ columns from the Oslo CTM2 are also evaluated for stratospheric correction.

Our study shows that stratospheric NO₂ columns from SCIAMACHY limb measurements very well reflect stratospheric conditions. The zonal variability of the stratospheric NO₂ field is captured by our matching algorithm, and the quality of the resulting tropospheric NO₂ columns improves considerably. Both stratospheric datasets need to be adjusted to the level of the nadir measurements, because a time- and latitude-dependent bias to the measured nadir columns can be observed over clean regions. After this offset is removed, the two datasets agree remarkably well, and both stratospheric correction methods provide a significant improvement to the retrieval of tropospheric NO₂ columns from the SCIAMACHY instrument.