ENVISAT/SCIAMACHY VALIDATION WITH THE LPMA/DOAS/MINI-DOAS BALLOON GONDOLA: COMPARISON OF O3, NO2 AND BRO PROFILES

被引:0
作者
Dorf, Marcel [1 ]
Kritten, Lena [1 ]
Kreycy, Sebastian [1 ]
Rozanov, Alexei [2 ]
Butz, Andre [3 ]
von Savigny, Christian [2 ]
Camy-Peyret, Claude [4 ]
Chipperfield, Martyn P. [5 ]
Grunow, Katja [6 ]
Prados-Roman, Cristina [1 ]
Burrows, John P. [2 ]
Pfeilsticker, Klaus [1 ]
机构
[1] Heidelberg Univ, Inst Environm Phys, INF 229, D-69120 Heidelberg, Germany
[2] Univ Bremen, Inst Environm Phys, D-28359 Bremen, Germany
[3] SRON, Netherlands Inst Space Res, NL-3584 CA Utrecht, Netherlands
[4] Univ Paris 06, LPMAA, F-75252 Paris, France
[5] Univ Leeds, Sch Earth & Environm, Inst Atomspher Sci, Leeds LS2 9JT, W Yorkshire, England
[6] Free Univ Berlin, Inst Meteorol, D-12165 Berlin, Germany
来源
PROCEEDINGS OF THE 19TH ESA SYMPOSIUM ON EUROPEAN ROCKET AND BALLOON PROGRAMMES AND RELATED RESEARCH | 2009年 / 671卷
关键词
SPECTROSCOPY;
D O I
暂无
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
Level 2 products (profiles of O-3, NO2, BrO) of the Envisat/SCIAMACHY instrument are validated by balloon-borne measurements of the same quantities using the same optical technique. The comparison studies with the level 2 retrievals of the University of Bremen are encouraging. Generally, the satellite and the balloon-borne O-3 retrievals agree within 15 to 20 % above 15 km. For NO2, a good agreement within about 20% is observed down to 18 km. At lower altitudes the relative differences increase, reaching about 40% at 15 km. For BrO we revisit the study of [1] which validates the scientific BrO product. A good agreement within about 20% is found between 15 and 25 km for measurements at mid and high-latitudes. The comparison for a tropical balloon flight shows, however, larger discrepancies of about 20-50%.
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收藏
页码:169 / 174
页数:6
相关论文
共 14 条
[1]  
Bovensmann H, 1999, J ATMOS SCI, V56, P127, DOI 10.1175/1520-0469(1999)056<0127:SMOAMM>2.0.CO
[2]  
2
[3]   Inter-comparison of stratospheric O3 and NO2 abundances retrieved from balloon borne direct sun observations and Envisat/SCIAMACHY limb measurements [J].
Butz, A ;
Bösch, H ;
Camy-Peyret, C ;
Chipperfield, M ;
Dorf, M ;
Dufour, G ;
Grunow, K ;
Jeseck, P ;
Kühl, S ;
Payan, S ;
Pepin, I ;
Pukite, J ;
Rozanov, A ;
von Savigny, C ;
Sioris, C ;
Wagner, T ;
Weidner, F ;
Pfeilsticker, K .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :1293-1314
[4]   BALLOON-BORNE INFRARED FOURIER-TRANSFORM SPECTROSCOPY FOR MEASUREMENTS OF ATMOSPHERIC TRACE SPECIES [J].
CAMYPEYRET, C .
SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY, 1995, 51 (07) :1143-1152
[5]   Multiannual simulations with a three-dimensional chemical transport model [J].
Chipperfield, MP .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D1) :1781-1805
[6]   Balloon-borne stratospheric BrO measurements:: comparison with Envisat/SCIAMACHY BrO limb profiles [J].
Dorf, M. ;
Boesch, H. ;
Butz, A. ;
Camy-Peyret, C. ;
Chipperfield, M. P. ;
Engel, A. ;
Goutail, F. ;
Grunow, K. ;
Hendrick, F. ;
Hrechanyy, S. ;
Naujokat, B. ;
Pommereau, J. -P. ;
Van Roozendael, M. ;
Sioris, C. ;
Stroh, F. ;
Weidner, F. ;
Pfeilsticker, K. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :2483-2501
[7]   Differential optical absorption spectroscopy instrument for stratospheric balloonborne trace-gas studies [J].
Ferlemann, F ;
Bauer, N ;
Fitzenberger, R ;
Harder, H ;
Osterkamp, H ;
Perner, D ;
Platt, U ;
Schneider, M ;
Vradelis, P ;
Pfeilsticker, K .
APPLIED OPTICS, 2000, 39 (15) :2377-2386
[8]  
Grunow K., 2008, THESIS
[9]   SYNOPTIC ANALYSIS AND TRAJECTORIES DURING THE MAP-GLOBUS CAMPAIGN 1983 [J].
LANGEMATZ, U ;
LABITZKE, K ;
REIMER, E .
PLANETARY AND SPACE SCIENCE, 1987, 35 (05) :525-538
[10]  
Platt U., 2006, DIFFERENTIAL OPTICAL