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Geostationary Satellites Total Ozone Observations: First Results on Ground‐Based Networks Validation Efforts for TEMPO and GEMS
Título : Geostationary Satellites Total Ozone Observations: First Results on Ground‐Based Networks Validation Efforts for TEMPO and GEMS
Autor : Zhao, XiaoyiGriffin, DeboraFioletov, VitaliMcLinden, ChrisLiu, XiongPark, JunsungPetropavlovskikh, IrinaHanisco, Thomas F.Szykman, JamesValin, LukasBaumann, EricCede, AlexanderTiefengraber, MartinGebetsberger, ManuelUesato, ItaruZheng, XiangdongAhn, SoiChang, LimseokLee, Won‐JinKim, Jae HwanLee, HyunjinBaek, KanghyunRedondas, Alberto ORCID RESEARCHERID Autor AEMETFujiwara, MasatomoWang, TingGrutter, MichelHouck, John C.Haffner, DavidLee, Sum Chi
Palabras clave : Geostationary Satellites; Ozone Observations; Monitoring of Pollution; TEMPO; GEMS
Fecha de publicación : 2025
Editor: Wiley; American Geophysical Union
Citación : Geophysical Research Letters. 2025, 52(12), e2025GL114768
Versión del editor: https://doi.org/10.1029/2025GL114768
Resumen : The Tropospheric Emissions: Monitoring of Pollution (TEMPO) instrument, launched in April 2023, is North America's first geostationary air pollution monitoring satellite mission. Together with Asia's Geostationary Environment Monitoring Spectrometer (GEMS) launched in 2020 and Europe's upcoming Sentinel-4, TEMPO contributes to nearly global coverage provided by geostationary satellite constellation. TEMPO and GEMS offer hourly, high-resolution data of ozone surpassing the once-daily observations of instruments like the TROPOspheric Monitoring Instrument (TROPOMI) in temporal resolution. This study presents TEMPO's total ozone data, demonstrating TEMPO's ability to observe sudden changes in ozone and UV index. Furthermore, TEMPO and GEMS measurements are validated using ground-based monitoring networks (Brewer, Dobson, and Pandora). Results show good agreement but also highlight latitude-dependent discrepancies between the satellite and ground-based data sets (−2% to 2% for TEMPO, −1% to −3% for GEMS). Findings are further validated using TROPOMI data and reanalysis models.
Patrocinador: Irina Petropavlovskikh's research was supported by a NOAA Cooperative Agreement with CIRES, NA17OAR4320101. The Mexican Pandora instruments and operation were financed through Grants by AEM-CONAHCYT (275239) and UNAM-DGAPA (IG101225). SAO coauthors were supported by the NASA TEMPO project (Contract NNL13AA09C), as well as the NASA Grant 80NSSC19K1626. We thank Dr. Peter Effertz at CIRES, University of Colorado, for generating temperature-corrected Dobson data for the U.S. sites.
URI : http://hdl.handle.net/20.500.11765/16797
ISSN : 0094-8276
1944-8007
Colecciones: Artículos científicos 2023-2026


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