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NO(2) retrievals from NOAA-20 OMPS: Algorithm, evaluation, and observations of drastic changes during COVID-19

We present the first NO(2) 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 km(2) similar to the Ozone Monitoring Instrument (OMI). The retrieval of NO...

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Detalles Bibliográficos
Autores principales: Huang, Xinzhou, Yang, Kai, Kondragunta, Shobha, Wei, Zigang, Valin, Lucas, Szykman, James, Goldberg, Mitch
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Published by Elsevier Ltd. 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9441478/
https://www.ncbi.nlm.nih.gov/pubmed/36092473
http://dx.doi.org/10.1016/j.atmosenv.2022.119367
Descripción
Sumario:We present the first NO(2) 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 km(2) similar to the Ozone Monitoring Instrument (OMI). The retrieval of NOAA-20 NO(2) vertical columns were achieved through the Direct Vertical Column Fitting (DVCF) algorithm, which was uniquely designed and successfully used to retrieve NO(2) 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 NO(2) in January–April 2020 due to COVID-19 lockdown, consistent with the findings from other satellite observations. The NO(2) 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 NO(2) total columns, but generally the agreement is within ±2.5 × 10(15) molecules/cm(2). Comparisons of stratospheric NO(2) 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 NO(2) and highlight its potential use for extending the long-term global NO(2) record.