NO2 retrievals from NOAA-20 OMPS: Algorithm, evaluation, and observations of drastic changes during COVID-19

Xinzhou Huang; Kai Yang; Shobha Kondragunta; Zigang Wei; Lucas Valin; James Szykman; Mitch Goldberg

doi:10.1016/j.atmosenv.2022.119367

NO₂ retrievals from NOAA-20 OMPS: Algorithm, evaluation, and observations of drastic changes during COVID-19

Atmos Environ (1994). 2022 Sep 5:119367. doi: 10.1016/j.atmosenv.2022.119367. Online ahead of print.

Authors

Xinzhou Huang¹, Kai Yang¹, Shobha Kondragunta², Zigang Wei³, Lucas Valin⁴, James Szykman⁵, Mitch Goldberg²

Affiliations

¹ Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD, USA.
² NOAA NESDIS, College Park, MD, USA.
³ IMSG at NOAA, College Park, MD, USA.
⁴ US EPA, ORD, Center for Environmental Measurements and Modeling, Research Triangle Park, NC, USA.
⁵ US EPA, ORD, Center for Environmental Measurements and Modeling, Hampton, VA, USA.

Abstract

We present the first NO₂ measurements from the Nadir Mapper of Ozone Mapping and Profiler Suite (OMPS) instrument aboard the NOAA-20 satellite. NOAA-20 OMPS was launched in November 2017, with a nadir resolution of 17 × 13 km² similar to the Ozone Monitoring Instrument (OMI). The retrieval of NOAA-20 NO₂ vertical columns were achieved through the Direct Vertical Column Fitting (DVCF) algorithm, which was uniquely designed and successfully used to retrieve NO₂ from OMPS aboard Suomi National Polar-orbiting Partnership (SNPP) spacecraft, predecessor to NOAA-20. Observations from NOAA-20 reveal a 20-40% decline in regional tropospheric NO₂ in January-April 2020 due to COVID-19 lockdown, consistent with the findings from other satellite observations. The NO₂ retrievals are preliminarily validated against ground-based Pandora spectrometer measurements over the New York City area as well as other U.S. Pandora locations. It shows OMPS total columns tend to be lower in polluted urban regions and higher in clean areas/episodes associated with relatively small NO₂ total columns, but generally the agreement is within ±2.5 × 10¹⁵ molecules/cm². Comparisons of stratospheric NO₂ columns exhibit the excellent agreement between OMPS and OMI, validating OMPS capability in capturing the stratospheric background accurately. These results demonstrate the high sensitivity of OMPS to tropospheric NO₂ and highlight its potential use for extending the long-term global NO₂ record.

Keywords: COVID-19; NOAA-20; OMPS; Stratosphere and troposphere NO2.