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dc.contributor.authorNowlan, C.R.
dc.contributor.authorGonzález Abad, G.
dc.contributor.authorKwon, H.-A.
dc.contributor.authorAyazpour, Z.
dc.contributor.authorChan Miller, C.
dc.contributor.authorChance, K.
dc.contributor.authorChong, H.
dc.contributor.authorLiu, X.
dc.contributor.authorO’Sullivan, E.
dc.contributor.authorWang, H.
dc.contributor.authorZhu, L.
dc.contributor.authorDe Smedt, I.
dc.contributor.authorJaross, G.
dc.contributor.authorSeftor, C.
dc.contributor.authorSun, K.
dc.date2023
dc.date.accessioned2023-05-17T04:41:35Z
dc.date.available2023-05-17T04:41:35Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/10993
dc.descriptionWe describe new publicly available, multi-year formaldehyde (HCHO) data records from the Ozone Mapping and Profiler Suite (OMPS) nadir mapper (NM) instruments on the Suomi NPP and NOAA-20 satellites. The OMPS-NM instruments measure backscattered UV light over the globe once per day, with spatial resolutions close to nadir of 50 × 50 km2 (OMPS/Suomi-NPP) and 17 × 17 km2 or 12 × 17 km2 (OMPS/NOAA-20). After a preliminary instrument line shape and wavelength calibration using on-orbit observations, we use the backscatter measurements in a direct spectral fit of radiances, in combination with a nadir reference spectrum collected over a clean area, to determine slant columns of HCHO. The slant columns are converted to vertical columns using air mass factors (AMFs) derived through scene-by-scene radiative transfer calculations. Finally, a correction is applied to account for background HCHO in the reference spectrum, as well as any remaining high-latitude biases. We investigate the consistency of the OMPS products from Suomi NPP and NOAA-20 using long-term monthly means over 12 geographic regions, and also compare the products with publicly available TROPOMI HCHO observations. OMPS/Suomi-NPP and OMPS/NOAA-20 monthly mean HCHO vertical columns are highly consistent (r = 0.98), with low proportional (2\%) and offset (2 × 1014 molecules cm−2) biases. OMPS HCHO monthly means are also well-correlated with those from TROPOMI (r = 0.92), although they are consistently 10\% ± 16\% larger in polluted regions (columns >8 × 1015 molecules cm−2). These differences result primarily from differences in AMFs.
dc.languageeng
dc.titleGlobal Formaldehyde Products From the Ozone Mapping and Profiler Suite (OMPS) Nadir Mappers on Suomi NPP and NOAA-20
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeOMPS
dc.subject.freeJPSS
dc.subject.freeformaldehyde
dc.subject.freevolatile organic compounds
dc.subject.freeSuomi NPP
dc.subject.freeNOAA-20
dc.source.titleEarth and Space Science
dc.source.volume10
dc.source.issue5
dc.source.pagee2022EA002643
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/2022EA002643
dc.identifier.scopus


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