CO measurements from the ACE-FTS satellite instrument:: data analysis and validation using ground-based, airborne and spaceborne observations

被引:70
作者
Clerbaux, C. [1 ]
George, M. [1 ]
Turquety, S. [1 ]
Walker, K. A. [2 ,3 ]
Barret, B. [4 ]
Bernath, P. [2 ,5 ]
Boone, C. [2 ]
Borsdorff, T. [6 ]
Cammas, J. P. [4 ]
Catoire, V. [7 ]
Coffey, M. [8 ]
Coheur, P. -F. [9 ]
Deeter, M. [8 ]
De Maziere, M. [10 ]
Drummond, J. [11 ]
Duchatelet, P. [12 ]
Dupuy, E. [2 ]
de Zafra, R. [13 ]
Eddounia, F. [1 ]
Edwards, D. P. [8 ]
Emmons, L. [8 ]
Funke, B. [14 ]
Gille, J. [8 ]
Griffith, D. W. T. [15 ]
Hannigan, J. [8 ]
Hase, F. [16 ]
Hoepfner, M. [16 ]
Jones, N. [15 ]
Kagawa, A. [17 ]
Kasai, Y. [18 ]
Kramer, I. [16 ]
Le Flochmoen, E. [4 ]
Livesey, N. J. [19 ]
Lopez-Puertas, M. [14 ]
Luo, M. [20 ]
Mahieu, E. [12 ]
Murtagh, D. [21 ]
Nedelec, P. [4 ]
Pazmino, A. [1 ]
Pumphrey, H. [22 ]
Ricaud, P. [4 ]
Rinsland, C. P. [23 ]
Robert, C. [7 ]
Schneider, M. [16 ]
Senten, C. [10 ]
Stiller, G. [16 ]
Strandberg, A. [21 ]
Strong, K. [3 ]
Sussmann, R. [6 ]
Thouret, V. [4 ]
机构
[1] Univ Paris 06, CNRS, Serv Aeron IPSL, Paris, France
[2] Univ Waterloo, Dept Chem, Waterloo, ON N2L 3G1, Canada
[3] Univ Toronto, Dept Phys, Toronto, ON M5S 1A7, Canada
[4] Observ Midi Pyrenees, UMR 5560, Lab Aerol, F-31400 Toulouse, France
[5] Univ York, Dept Chem, York YO10 5DD, N Yorkshire, England
[6] IMK IFU, Forschungszentrum Karlsruhe, Garmisch Partenkirchen, Germany
[7] Univ Orleans, CNRS, Lab Phys & Chim Environm, Orleans, France
[8] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[9] Univ Libre Bruxelles, Brussels, Belgium
[10] Belgian Inst Space Aeron, Brussels, Belgium
[11] Dalhousie Univ, Dept Phys & Atmospher Sci, Halifax, NS, Canada
[12] Univ Liege, Inst Astrophys & Geophys, Liege, Belgium
[13] SUNY Stony Brook, Dept Phys & Astron, Stony Brook, NY 11794 USA
[14] CSIC, Inst Astrofis Andalucia, Granada, Spain
[15] Univ Wollongong, Dept Chem, Wollongong, NSW 2500, Australia
[16] Forschungszentrum Karlsruhe, Inst Meteorol & Klimaforsch, Karlsruhe, Germany
[17] Fujitsu FIP Corp, Tokyo, Japan
[18] Natl Inst Informat & Commun Technol, Tokyo, Japan
[19] Jet Prop Lab, Microwave Atmospher Sci Team, Pasadena, CA USA
[20] CALTECH, Jet Prop Lab, Pasadena, CA USA
[21] Chalmers Univ Technol, S-41296 Gothenburg, Sweden
[22] Sch GeoSci, Edinburgh, Midlothian, Scotland
[23] NASA, Langley Res Ctr, Hampton, VA 23665 USA
关键词
D O I
10.5194/acp-8-2569-2008
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Atmospheric Chemistry Experiment (ACE) mission was launched in August 2003 to sound the atmosphere by solar occultation. Carbon monoxide (CO), a good tracer of pollution plumes and atmospheric dynamics, is one of the key species provided by the primary instrument, the ACE-Fourier Transform Spectrometer (ACE-FTS). This instrument performs measurements in both the CO 1-0 and 2-0 ro-vibrational bands, from which vertically resolved CO concentration profiles are retrieved, from the mid-troposphere to the thermosphere. This paper presents an updated description of the ACE-FTS version 2.2 CO data product, along with a comprehensive validation of these profiles using available observations (February 2004 to December 2006). We have compared the CO partial columns with ground-based measurements using Fourier transform infrared spectroscopy and millimeter wave radiometry, and the volume mixing ratio profiles with airborne (both high-altitude balloon flight and airplane) observations. CO satellite observations provided by nadir-looking instruments (MOPITT and TES) as well as limb-viewing remote sensors (MIPAS, SMR and MLS) were also compared with the ACE-FTS CO products. We show that the ACE-FTS measurements provide CO profiles with small retrieval errors (better than 5% from the upper troposphere to 40 km, and better than 10% above). These observations agree well with the correlative measurements, considering the rather loose coincidence criteria in some cases. Based on the validation exercise we assess the following uncertainties to the ACE-FTS measurement data: better than 15% in the upper troposphere (8-12 km), than 30% in the lower stratosphere (12-30 km), and than 25% from 30 to 100 km.
引用
收藏
页码:2569 / 2594
页数:26
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