Stratospheric profiles of nitrogen dioxide observed by Optical Spectrograph and Infrared Imager System on the Odin satellite -: art. no. 4215

被引:49
作者
Sioris, CE
Haley, CS
McLinden, CA
von Savigny, C
McDade, IC
McConnell, JC
Evans, WFJ
Lloyd, ND
Llewellyn, EJ
Chance, KV
Kurosu, TP
Murtagh, D
Frisk, U
Pfeilsticker, K
Bösch, H
Weidner, F
Strong, K
Stegman, J
Mégie, G
机构
[1] Harvard Smithsonian Ctr Astrophys, Atom & Mol Phys Div, Cambridge, MA 02138 USA
[2] Heidelberg Univ, Inst Environm Phys, D-69120 Heidelberg, Germany
[3] Trent Univ, Dept Phys, Peterborough, ON K9J 7B8, Canada
[4] Swedish Space Corp, SE-17104 Solna, Sweden
[5] York Univ, Ctr Earth & Space Sci, Toronto, ON M3J 2R7, Canada
[6] Univ Saskatchewan, Dept Phys & Engn Phys, Saskatoon, SK S7N 5E2, Canada
[7] Environm Canada, Meteorol Serv Canada, Toronto, ON, Canada
[8] Univ Paris 06, IPSL, CNRS, Serv Aeron, F-75252 Paris 05, France
[9] Chalmers Univ, Dept Radio & Space Sci, SE-41296 Gothenburg, Sweden
[10] Stockholm Univ, Dept Meteorol, SE-10691 Stockholm, Sweden
[11] Univ Toronto, Dept Phys, Toronto, ON M5S 1A7, Canada
[12] Univ Bremen, Inst Environm Phys, D-28359 Bremen, Germany
关键词
optical; Sun-synchronous; polar-orbiting; Fraunhofer; Ring effect; iterative onion peel;
D O I
10.1029/2002JD002672
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] Vertical profiles of nitrogen dioxide in the 19-40 km altitude range are successfully retrieved over the globe from Optical Spectrograph and Infrared Imager System (OSIRIS) limb scatter observations in late 2001 and early 2002. The inclusion of multiple scattering in the radiative transfer model used in the inversion algorithm allows for the retrieval of NO2 down to 19 km. The slant column densities, which represent the observations in the inversion, are obtained by fitting the fine structure in normalized radiance spectra over the 435-449 nm range, where NO2 electronic absorption is readily observable because of long light paths through stratospheric layers rich in this constituent. Details of the spectral fitting and inversion algorithm are discussed, including the discovery of a pseudo-absorber associated with pixelated detectors and a new method to verify altitude registration. Comparisons are made with spatially and temporally coincident profile measurements of this photochemically active trace gas. Better than 20% agreement is obtained with all correlative measurements over the common retrieval altitude range, confirming the validity of OSIRIS NO2 profiles. Systematic biases in the number densities are not observed at any altitude. A "snapshot'' meridional cross section between 40degreesN and 70degreesS is shown from observations during a fraction of an orbit.
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页数:19
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