Stratospheric ozone profiles retrieved from limb scattered sunlight radiance spectra measured by the OSIRIS instrument on the Odin satellite -: art. no. 1755

被引:76
作者
von Savigny, C
Haley, CS
Sioris, CE
McDade, IC
Llewellyn, EJ
Degenstein, D
Evans, WFJ
Gattinger, RL
Griffioen, E
Kyrölä, E
Lloyd, ND
McConnell, JC
McLinden, CA
Mégie, G
Murtagh, DP
Solheim, B
Strong, K
机构
[1] York Univ, CRESS, Toronto, ON M3J 2R7, Canada
[2] Univ Saskatchewan, Dept Phys & Engn Phys, Saskatoon, SK, Canada
[3] Trent Univ, Dept Phys, Peterborough, ON K9J 7B8, Canada
[4] Finnish Meteorol Inst, FIN-00101 Helsinki, Finland
[5] Meteorol Serv Canada, ARQX, Toronto, ON, Canada
[6] Univ Paris 06, CNRS, IPSL Serv Aeron, Paris 5, France
[7] Chalmers Univ Technol, Dept Radio & Space Sci, S-41296 Gothenburg, Sweden
[8] Univ Toronto, Dept Phys, Toronto, ON, Canada
关键词
D O I
10.1029/2002GL016401
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
[1] Stratospheric ozone density profiles between 15 and 40 km altitude are derived from scattered sunlight limb radiance spectra measured with the Optical Spectrograph and InfraRed Imager System (OSIRIS) on the Odin satellite. The method is based on the analysis of limb radiance profiles in the centre and the wings of the Chappuis-Wulf absorption bands of ozone. It employs a non-linear Newtonian iteration version of Optimal Estimation (OE) coupled with the radiative transfer model LIMBTRAN. The derived zonally averaged ozone field for August 2001 is in excellent agreement with the main characteristics of the global morphology of stratospheric ozone, indicating that the limb scatter technique is capable of providing ozone profiles with high accuracy and high vertical resolution on a global scale and a daily basis.
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页码:ASC8 / 1
页数:4
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