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Validation of OMPS Suomi NPP and OMPS NOAA-20 Formaldehyde Total Columns With NDACC FTIR Observations

  • H. A. Kwon
  • , G. González Abad
  • , C. R. Nowlan
  • , H. Chong
  • , A. H. Souri
  • , C. Vigouroux
  • , A. Röhling
  • , R. Kivi
  • , M. Makarova
  • , J. Notholt
  • , M. Palm
  • , H. Winkler
  • , Y. Té
  • , R. Sussmann
  • , M. Rettinger
  • , E. Mahieu
  • , K. Strong
  • , E. Lutsch
  • , S. Yamanouchi
  • , T. Nagahama
  • J. W. Hannigan, M. Zhou, I. Murata, M. Grutter, W. Stremme, M. De Mazière, N. Jones, D. Smale, I. Morino
  • Center for Astrophysics | Harvard & Smithsonian
  • Royal Belgian Institute for Space Aeronomy
  • Karlsruhe Institute of Technology
  • Finnish Meteorological Institute
  • St. Petersburg State University
  • University of Bremen
  • Sorbonne Université
  • University of Liege
  • University of Toronto
  • Nagoya University
  • National Center for Atmospheric Research
  • CAS - Institute of Atmospheric Physics
  • Tohoku University
  • Universidad Nacional Autónoma de México
  • University of Wollongong
  • NIWA
  • National Institute for Environmental Studies of Japan

Research output: Contribution to journalArticlepeer-review

16 Scopus citations

Abstract

We validate formaldehyde (HCHO) vertical column densities (VCDs) from Ozone Mapping and Profiler Suite Nadir Mapper (OMPS-NM) instruments onboard the Suomi National Polar-orbiting Partnership (Suomi NPP) satellite for 2012–2020 and National Oceanic and Atmospheric Administration-20 (NOAA-20) satellite for 2018–2020, hereafter referred to as OMPS-NPP and OMPS-N20, with ground-based Fourier-Transform Infrared (FTIR) observations of the Network for the Detection of Atmospheric Composition Change (NDACC). OMPS-NPP/N20 HCHO products reproduce seasonal variability at 24 FTIR sites. Monthly variability of OMPS-NPP/N20 has a very good agreement with FTIR, showing correlation coefficients of 0.83 and 0.88, respectively. OMPS-NPP (N20) biases averaged over all sites are −0.9 (4) ± 3 (6)%. However, at clean sites (with VCDs < 4.0 × 1015 molecules cm−2), positive biases of 20 (32) ± 6 (18)% occur for OMPS-NPP (N20). At sites with HCHO VCDs > 4.0 × 1015 molecules cm−2, negative biases of −15% ± 4% appear for OMPS-NPP, but OMPS-N20 shows smaller bias of 0.5% ± 6% due to its smaller ground pixel footprints. Therefore, smaller satellite footprint sizes are important in distinguishing small-scale plumes. In addition, we discuss a bias correction and provide lower limit for the monthly uncertainty of OMPS-NPP/N20 HCHO products. The total uncertainty for OMPS-NPP (N20) at clean sites is 0.7 (0.8) × 1015 molecules cm−2, corresponding to a relative uncertainty of 32 (30)%. In the case of HCHO VCDs > 4.0 × 1015 molecules cm−2, however, the relative uncertainty in HCHO VCDs for OMPS-NPP (N20) decreases to 31 (18)%.

Original languageEnglish
Article numbere2022EA002778
JournalEarth and Space Science
Volume10
Issue number5
DOIs
StatePublished - May 2023

Keywords

  • FTIR
  • NOAA-20
  • OMPS
  • Suomi NPP
  • formaldehyde
  • validation

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