Ozone comparison between Pandora #34, Dobson #061, OMI, and OMPS in Boulder, Colorado, for the period December 2013-December 2016
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2017
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Source Atmospheric Measurement Techniques, 10(9), 3539-3545.
Herman, J., Evans, R., Cede, A., Abuhassan, N., Petropavlovskikh, I., McConville, G., Miyagawa, K., & Noirot, B. (2017). Ozone comparison between Pandora #34, Dobson #061, OMI, and OMPS in Boulder, Colorado, for the period December 2013-December 2016. Atmospheric Measurement Techniques, 10(9). https://doi.org/10.5194/amt-10-3539-2017
Herman, Jay, Robert Evans, Alexander Cede, Nader Abuhassan, Irina Petropavlovskikh, Glenn McConville, Koji Miyagawa, and Brandon Noirot. "Ozone comparison between Pandora #34, Dobson #061, OMI, and OMPS in Boulder, Colorado, for the period December 2013-December 2016." Atmospheric Measurement Techniques 10, no. 9 (2017). https://doi.org/10.5194/amt-10-3539-2017.
Herman, Jay, et al. "Ozone comparison between Pandora #34, Dobson #061, OMI, and OMPS in Boulder, Colorado, for the period December 2013-December 2016." Atmospheric Measurement Techniques, vol. 10, no. 9, 2017. NOAA IR. https://doi.org/10.5194/amt-10-3539-2017.
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Journal Title:Atmospheric Measurement Techniques
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NOAA Program & Office:
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Description:A one-time-calibrated (in December 2013) Pandora spectrometer instrument (Pan #034) has been compared to a periodically calibrated Dobson spectroradiometer (Dobson #061) co-located in Boulder, Colorado, and compared with two satellite instruments over a 3-year period (December 2013-December 2016). The results show good agreement between Pan #034 and Dobson #061 within their statistical uncertainties. Both records are corrected for ozone retrieval sensitivity to stratospheric temperature variability obtained from the Global Modeling Initiative (GMI) and Modern-Era Retrospective analysis for Research and Applications (MERRA-2) model calculations. Pandora #034 and Dobson #061 differ by an average of 2.1 +/- 3.2% when both instruments use their standard ozone absorption cross sections in the retrieval algorithms. The results show a relative drift (0.2 +/- 0.08% yr(-1)) between Pandora observations against NOAA Dobson in Boulder, CO, over a 3-year period of continuous operation. Pandora drifts relative to the satellite Ozone Monitoring Instrument (OMI) and the Ozone Mapping Profiler Suite (OMPS) are +0.18 +/- 0.2% yr(-1) and -0.18 +/- 0.2% yr(-1), respectively, where the uncertainties are 2 standard deviations. The drift between Dobson #061 and OMPS for a 5.5-year period (January 2012-June 2017) is -0.07 +/- 0.06% yr(-1).
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Source:Atmospheric Measurement Techniques, 10(9), 3539-3545.
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Rights Information:CC BY
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Herman, J., Evans, R., Cede, A., Abuhassan, N., Petropavlovskikh, I., McConville, G., Miyagawa, K., & Noirot, B. (2017). Ozone comparison between Pandora #34, Dobson #061, OMI, and OMPS in Boulder, Colorado, for the period December 2013-December 2016. Atmospheric Measurement Techniques, 10(9). https://doi.org/10.5194/amt-10-3539-2017
Herman, Jay, Robert Evans, Alexander Cede, Nader Abuhassan, Irina Petropavlovskikh, Glenn McConville, Koji Miyagawa, and Brandon Noirot. "Ozone comparison between Pandora #34, Dobson #061, OMI, and OMPS in Boulder, Colorado, for the period December 2013-December 2016." Atmospheric Measurement Techniques 10, no. 9 (2017). https://doi.org/10.5194/amt-10-3539-2017.
Herman, Jay, et al. "Ozone comparison between Pandora #34, Dobson #061, OMI, and OMPS in Boulder, Colorado, for the period December 2013-December 2016." Atmospheric Measurement Techniques, vol. 10, no. 9, 2017. NOAA IR. https://doi.org/10.5194/amt-10-3539-2017.
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