Validation of POLDER/ADEOS data using a ground-based lidar network: Preliminary results for cirrus clouds

被引:8
作者
Chepfer, H [1 ]
Goloub, P
Sauvage, L
Flamant, PH
Brogniez, G
Spinhirne, J
Lavorato, M
Sugimoto, N
Pelon, J
机构
[1] Ecole Polytech, Inst Pierre Simon Laplace, Meteorol Dynam Lab, F-91128 Palaiseau, France
[2] Univ Lille 1, Opt Atmospher Lab, F-59655 Villeneuve Dascq, France
[3] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[4] CONICET, CEILAP, CITELA, Villa Martelli, Argentina
[5] Natl Inst Environm Studies, Tsukuba, Ibaraki, Japan
来源
PHYSICS AND CHEMISTRY OF THE EARTH PART B-HYDROLOGY OCEANS AND ATMOSPHERE | 1999年 / 24卷 / 03期
关键词
D O I
10.1016/S1464-1909(98)00038-0
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
POLDER-1 on board the Japanese ADEOS platform has collected 8 months of data (October 1996 to June 1997). POLDER is a visible radiometer with multi-directional and polarization capabilities. These features allow to obtain information both on cloud thermodynamical phase and cloud altitude. The POLDER cloud algorithms are currently under validation. For cirrus clouds, a validation based on a comparison between cloud properties inferred from POLDER-1 data and cloud properties retrieved from a ground-based lidar network is currently under consideration. In this paper, preliminary comparisons between cloud altitude inferred from POLDER-1 and lidars are presented. These comparisons show an underestimation of cloud altitude by POLDER-1 for optically thin clouds. A first theoretical analysis based on radiative transfer simulations allows to explain the difference between POLDER and lidar altitudes. Moreover. a preliminary comparison between thermodynamical cloud phase (liquid water / ice) obtained with POLDER-1 and cloud temperature inferred from radiosoundings and cloud altitudes shows that cirrus clouds at temperatures lower than -40 degrees C are correctly identified as ice layers by POLDER-1 (C) 1999 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:203 / 206
页数:4
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