Improvements to the retrieval of tropospheric NO<sub>2</sub> from satellite – stratospheric correction using SCIAMACHY limb/nadir matching and comparison to Oslo CTM2 simulations
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 (NO<sub>2&...
| Main Authors: | , , , , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2013-03-01
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| Series: | Atmospheric Measurement Techniques |
| Online Access: | http://www.atmos-meas-tech.net/6/565/2013/amt-6-565-2013.pdf |
| Summary: | 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 (NO<sub>2</sub>), it is necessary to separate the stratospheric from the tropospheric signal. <br><br> 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 NO<sub>2</sub> abundances to correct the nadir measurements' total columns. <br><br> In this manuscript, we present a novel approach to limb/nadir matching, calculating one stratospheric NO<sub>2</sub> value from limb measurements for every single nadir measurement, abandoning global coverage for the sake of spatial accuracy. For comparison, modelled stratospheric NO<sub>2</sub> columns from the Oslo CTM2 are also evaluated for stratospheric correction. <br><br> Our study shows that stratospheric NO<sub>2</sub> columns from SCIAMACHY limb measurements very well reflect stratospheric conditions. The zonal variability of the stratospheric NO<sub>2</sub> field is captured by our matching algorithm, and the quality of the resulting tropospheric NO<sub>2</sub> 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 NO<sub>2</sub> columns from the SCIAMACHY instrument. |
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| ISSN: | 1867-1381 1867-8548 |