Detection of high clouds in polar regions during the daytime using the MODIS 1.375-μm channel

被引:24
作者
Gao, BC [1 ]
Yang, P
Li, RR
机构
[1] USN, Res Lab, Remote Sensing Div, Washington, DC 20375 USA
[2] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA
[3] NASA, Goddard Space Flight Ctr, Sci Syst & Applicat Inc, Greenbelt, MD 20771 USA
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2003年 / 41卷 / 02期
关键词
atmosphere; cirrus cloud; remote sensing;
D O I
10.1109/TGRS.2002.808290
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Identification of clouds over earth's polar regions is difficult from satellite radiometric measurements in the visible and infrared (IR) atmospheric window regions because of the high albedos of snow- and ice-covered surfaces in the visible and the low-temperature contrast between the surface and the troposphere in the IR. The Moderate Resolution Imaging SpectroRadiometer (MODIS) on the Terra Spacecraft has a near-IR channel located within the strong water vapor absorption regions close to 1.38 mum. This channel was originally designed for remote sensing of high-altitude clouds in the tropical and mid-latitude regions. In this paper, we report that this channel is also quite useful for detecting high clouds in polar regions during the daytime. Comparisons with IR emission techniques for polar cloud detections are also presented.
引用
收藏
页码:474 / 481
页数:8
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