Cross-validation of MIPAS/ENVISAT and GPS-RO/CHAMP temperature profiles -: art. no. D19311

被引:22
|
作者
Wang, DY
Stiller, GP
von Clarmann, T
Fischer, H
López-Puertas, M
Funke, B
Glatthor, N
Grabowski, U
Höpfner, M
Kellmann, S
Kiefer, M
Linden, A
Tsidu, GM
Milz, M
Steck, T
Jiang, JH
Ao, CO
Manney, G
Hocke, K
Wu, DL
Romans, LJ
Wickert, J
Schmidt, T
机构
[1] Forschungszentrum Karlsruhe, Inst Meteorol & Klimaforsch, D-76021 Karlsruhe, Germany
[2] Univ Karlsruhe, D-76021 Karlsruhe, Germany
[3] CSIC, Inst Astrofis Andalucia, E-18008 Granada, Spain
[4] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[5] New Mexico Highlands Univ, Dept Nat Sci, Los Vegas, NM USA
[6] Max Planck Inst Aeron, D-37191 Katlenburg Lindau, Germany
[7] Geoforschungszentrum Potsdam, Dept Geodesy & Remote Sensing 1, D-14473 Potsdam, Germany
关键词
CHAMP; MIPAS; temperature;
D O I
10.1029/2004JD004963
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) on board the ENVISAT and the Global Positioning System (GPS) receiver on the Challenging Mini-Satellite Payload (CHAMP) provide temperature profiles by limb-viewing midinfrared emission and radio occultation (RO) measurements, respectively. The MIPAS temperatures retrieved at the Institut fur Meteorologie und Klimaforschung (IMK) are compared with the GPS-RO/CHAMP observations derived at Jet Propulsion Laboratory (JPL) and GeoForschungsZentrum (GFZ) Potsdam. The three data sets show generally good agreement. The global mean differences averaged between 8 and 30 km in 14 days of September/October 2002 are -0.44 +/- 0.02 K and 0.07 +/- 0.02 K for MIPAS/GPS-RO JPL and GFZ comparisons, respectively. The MIPAS global mean temperatures below 25 km are slightly lower than those of GPS-RO JPL and GFZ by less than 1 K and 0.2 K, respectively. Above 25 km, the MIPAS temperatures are higher than the JPL and GFZ data, in particular near both poles and the equator, with maxima of 1 K for JPL and 1.5 K for GFZ at 30 km. The standard deviations are similar to2-4 K. Possible explanations for the observed differences include (1) effect of spatial and temporal mismatch between the correlative measurements on the observed standard deviations, in particular in regions and episodes of enhanced wave activity; (2) a negative bias in GPS-RO/CHAMP temperatures in regions of increased humidity; (3) a mapping of initialization temperature profiles on GPS-RO/CHAMP retrievals at altitudes where low refraction contains no information on air density; and (4) measurement errors of both instruments, particularly the errors due to insufficient knowledge of the instrument line shape and spectroscopy in current MIPAS retrievals.
引用
收藏
页码:D193111 / 15
页数:15
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