Back to Search Start Over

Validation of Odin/OSIRIS stratospheric NO2 profiles

Authors :
Ghassan Taha
Larry L. Gordley
Ariane Bazureau
Edward J. Llewellyn
Jerry Lumpe
Cora E. Randall
Craig S. Haley
Larry W. Thomasson
Donal P. Murtagh
Samuel Brohede
S. V. Petelina
Christopher E. Sioris
Florence Goutail
Chris A. McLinden
Department of Radio and Space Science [Göteborg]
Chalmers University of Technology [Göteborg]
Centre for Research in Earth and Space Science [Toronto] (CRESS)
York University [Toronto]
Environment and Climate Change Canada
Department of Physics and Engineering Physics [Saskatoon]
University of Saskatchewan [Saskatoon] (U of S)
Service d'aéronomie (SA)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Laboratory for Atmospheric and Space Physics [Boulder] (LASP)
University of Colorado [Boulder]
Department of Atmospheric and Oceanic Sciences [Boulder] (ATOC)
Computational Physics, Inc.
Science Systems and Applications, Inc. [Lanham] (SSAI)
NASA Langley Research Center [Hampton] (LaRC)
GATS Inc.
Source :
Journal of Geophysical Research: Atmospheres, Journal of Geophysical Research: Atmospheres, American Geophysical Union, 2007, 112, pp.D07310. ⟨10.1029/2006JD007586⟩, Journal of Geophysical Research: Atmospheres, 2007, 112, pp.D07310. ⟨10.1029/2006JD007586⟩
Publication Year :
2007
Publisher :
HAL CCSD, 2007.

Abstract

This paper presents the validation study of stratospheric NO2 profiles retrieved from Odin/OSIRIS measurements of limb-scattered sunlight (version 2.4). The Optical Spectrograph and Infrared Imager System (OSIRIS) NO2 data set is compared to coincident solar occultation measurements by the Halogen Occultation Experiment (HALOE), Stratospheric Aerosol and Gas Experiment (SAGE) II, SAGE III, and Polar Ozone and Aerosol Measurement (POAM) III during the 2002–2004 period. Comparisons with seven Systeme d'Analyse par Observation Zenithal (SAOZ) balloon measurements are also presented. All comparisons show good agreement, with differences, both random and systematic, of less than 20% between 25 km and 35 km. Inconsistencies with SAGE III below 25 km are found to be caused primarily by diurnal effects from varying NO2 concentrations along the SAGE III line-of-sight. On the basis of the differences, the OSIRIS random uncertainty is estimated to be 16% between 15 km and 25 km, 6% between 25 km and 35 km, and 9% between 35 km and 40 km. The estimated systematic uncertainty is about 22% between 15 and 25 km, 11–21% between 25 km and 35 km, and 11–31% between 35 km and 40 km. The uncertainties for AM (sunrise) profiles are generally largest and systematic deviations are found to be larger at equatorial latitudes. The results of this validation study show that the OSIRIS NO2 profiles are well behaved, with reasonable uncertainty estimates between 15 km and 40 km. This unique NO2 data set, with more than hemispheric coverage and high vertical resolution will be of particular interest for studies of nitrogen chemistry in the middle atmosphere, which is closely linked to ozone depletion.

Details

Language :
English
ISSN :
2169897X and 21698996
Database :
OpenAIRE
Journal :
Journal of Geophysical Research: Atmospheres, Journal of Geophysical Research: Atmospheres, American Geophysical Union, 2007, 112, pp.D07310. ⟨10.1029/2006JD007586⟩, Journal of Geophysical Research: Atmospheres, 2007, 112, pp.D07310. ⟨10.1029/2006JD007586⟩
Accession number :
edsair.doi.dedup.....b583060b9a5da13bb3c3ac735b708143