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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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creator | Willame, Yannick Depiesse, Cédric Mason, Jonathon P. Thomas, Ian R. Patel, Manish R. Hathi, Brijen Leese, Mark R. Bolsée, David Wolff, Michael J. Trompet, Loïc Vandaele, Ann Carine Piccialli, Arianna Aoki, Shohei Ristic, Bojan Neefs, Eddy Beeckman, Bram Berkenbosch, Sophie Clairquin, Roland Mahieux, Arnaud Pereira, Nuno Robert, Séverine Viscardy, Sébastien Wilquet, Valérie Daerden, Frank Lopez-Moreno, José Juan Bellucci, Giancarlo |
description | 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. |
doi_str_mv | 10.1016/j.pss.2022.105504 |
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•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.</description><identifier>ISSN: 0032-0633</identifier><identifier>EISSN: 1873-5088</identifier><identifier>DOI: 10.1016/j.pss.2022.105504</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><ispartof>Planetary and space science, 2022-09, Vol.218, p.105504, Article 105504</ispartof><rights>2022 The Authors</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c340t-33436596fe32f1b5aea51985879c99755e57cff0c064910997b252d6ce8dc0773</citedby><cites>FETCH-LOGICAL-c340t-33436596fe32f1b5aea51985879c99755e57cff0c064910997b252d6ce8dc0773</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Willame, Yannick</creatorcontrib><creatorcontrib>Depiesse, Cédric</creatorcontrib><creatorcontrib>Mason, Jonathon P.</creatorcontrib><creatorcontrib>Thomas, Ian R.</creatorcontrib><creatorcontrib>Patel, Manish R.</creatorcontrib><creatorcontrib>Hathi, Brijen</creatorcontrib><creatorcontrib>Leese, Mark R.</creatorcontrib><creatorcontrib>Bolsée, David</creatorcontrib><creatorcontrib>Wolff, Michael J.</creatorcontrib><creatorcontrib>Trompet, Loïc</creatorcontrib><creatorcontrib>Vandaele, Ann Carine</creatorcontrib><creatorcontrib>Piccialli, Arianna</creatorcontrib><creatorcontrib>Aoki, Shohei</creatorcontrib><creatorcontrib>Ristic, Bojan</creatorcontrib><creatorcontrib>Neefs, Eddy</creatorcontrib><creatorcontrib>Beeckman, Bram</creatorcontrib><creatorcontrib>Berkenbosch, Sophie</creatorcontrib><creatorcontrib>Clairquin, Roland</creatorcontrib><creatorcontrib>Mahieux, Arnaud</creatorcontrib><creatorcontrib>Pereira, Nuno</creatorcontrib><creatorcontrib>Robert, Séverine</creatorcontrib><creatorcontrib>Viscardy, Sébastien</creatorcontrib><creatorcontrib>Wilquet, Valérie</creatorcontrib><creatorcontrib>Daerden, Frank</creatorcontrib><creatorcontrib>Lopez-Moreno, José Juan</creatorcontrib><creatorcontrib>Bellucci, Giancarlo</creatorcontrib><title>Calibration of the NOMAD-UVIS data</title><title>Planetary and space science</title><description>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.</description><issn>0032-0633</issn><issn>1873-5088</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp9j0tLxDAUhYMoWEd_gLviPvUmaV64GuprYHQWOm5DmiaYMk6HpAj-ezvUtavLufAdzofQNYGKABG3fXXIuaJA6ZQ5h_oEFURJhjkodYoKAEYxCMbO0UXOPQAIQWWBbhq7i22yYxz25RDK8dOXr5uX5T3efqzeys6O9hKdBbvL_urvLtD28eG9ecbrzdOqWa6xYzWMmLGaCa5F8IwG0nLrLSdacSW101py7rl0IYADUWsC06ulnHbCedU5kJItEJl7XRpyTj6YQ4pfNv0YAuYoaXozSZqjpJklJ-ZuZvw07Dv6ZLKLfu98F5N3o-mG-A_9CxwNVps</recordid><startdate>20220901</startdate><enddate>20220901</enddate><creator>Willame, Yannick</creator><creator>Depiesse, Cédric</creator><creator>Mason, Jonathon P.</creator><creator>Thomas, Ian R.</creator><creator>Patel, Manish R.</creator><creator>Hathi, Brijen</creator><creator>Leese, Mark R.</creator><creator>Bolsée, David</creator><creator>Wolff, Michael J.</creator><creator>Trompet, Loïc</creator><creator>Vandaele, Ann Carine</creator><creator>Piccialli, Arianna</creator><creator>Aoki, Shohei</creator><creator>Ristic, Bojan</creator><creator>Neefs, Eddy</creator><creator>Beeckman, Bram</creator><creator>Berkenbosch, Sophie</creator><creator>Clairquin, Roland</creator><creator>Mahieux, Arnaud</creator><creator>Pereira, Nuno</creator><creator>Robert, Séverine</creator><creator>Viscardy, Sébastien</creator><creator>Wilquet, Valérie</creator><creator>Daerden, Frank</creator><creator>Lopez-Moreno, José Juan</creator><creator>Bellucci, Giancarlo</creator><general>Elsevier Ltd</general><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20220901</creationdate><title>Calibration of the NOMAD-UVIS data</title><author>Willame, Yannick ; 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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.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.pss.2022.105504</doi><oa>free_for_read</oa></addata></record> |
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title | Calibration of the NOMAD-UVIS data |
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