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Calibration of the NOMAD-UVIS data
The Ultraviolet and VIsible Spectrometer (UVIS), covering the 200–650 nm range, is one of three spectrometers that comprise the NOMAD instrument on the ExoMars 2016 Trace Gas Orbiter (TGO). UVIS can operate in solar occultation, nadir and limb viewing mode and was designed to monitor ozone and aero...
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Published in: | Planetary and space science 2022-09, Vol.218, p.105504, Article 105504 |
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Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article |
Language: | English |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The Ultraviolet and VIsible Spectrometer (UVIS), covering the 200–650 nm range, is one of three spectrometers that comprise the NOMAD instrument on the ExoMars 2016 Trace Gas Orbiter (TGO). UVIS can operate in solar occultation, nadir and limb viewing mode and was designed to monitor ozone and aerosols in the Martian atmosphere. Here, we describe the calibration procedure to convert the UVIS raw data into a calibrated data product ready for scientific exploitation. The calibration includes the CCD offset and dark current subtraction, the wavelength assignment, the noise identification and removal, the smearing removal, and the radiance or transmittance conversion. A straylight correction, critical for some parts of the UVIS spectral range, is also applied during the data reduction process, which is described in more detail in two companion papers [Mason et al., 2022; Depiesse et al., In prep] corresponding to two different and independent methods giving consistent results. The solar occultation observations are converted into transmittance and are therefore self-calibrating, while nadir and limb measurements require an absolute radiometric calibration. A comparison with coincident nadir MRO/MARCI measurements is provided as a final validation and generally shows a ±10% agreement on the radiances measured by both instruments.
•Description of the calibration of UVIS measurements to produce level 1 data from raw data•CCD non-linearity correction, offset removal, dark current removal, Bad pixel removal, Smearing removal.•A straylight correction is also applied but described in companion papers.•Conversions: Pixel-wavelength assignment, Radiance (nadir) or Transmittance (occultation) conversion.•Radiometric comparison with coincident MRO/MARCI measurements, serving as validation for the radiance calibrated data. |
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ISSN: | 0032-0633 1873-5088 |
DOI: | 10.1016/j.pss.2022.105504 |