Cloud Detection in Nonpolar Regions for CERES Using TRMM VIRS and Terra and Aqua MODIS Data

被引:162
作者
Minnis, Patrick [1 ]
Trepte, Qing Z. [2 ]
Sun-Mack, Szedung [2 ]
Chen, Yan [2 ]
Doelling, David R. [1 ]
Young, David F. [1 ]
Spangenberg, Douglas A. [2 ]
Miller, Walter F. [2 ]
Wielicki, Bruce A. [1 ]
Brown, Ricky R. [2 ]
Gibson, Sharon C. [2 ]
Geier, Erika B. [1 ]
机构
[1] NASA, Langley Res Ctr, Sci Directorate, Hampton, VA 23681 USA
[2] Sci Syst & Applicat Inc, Hampton, VA 23666 USA
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2008年 / 46卷 / 11期
基金
美国国家航空航天局;
关键词
Cloud; cloud detection; cloud mask; Clouds and Earth's Radiant Energy System (CERES); Moderate Resolution Imaging Spectroradiometer (MODIS); Visible and Infrared Scanner (VIRS);
D O I
10.1109/TGRS.2008.2001351
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
Objective techniques have been developed to consistently identify cloudy pixels over nonpolar regions in multispectral imager data coincident with measurements taken by the Clouds and Earth's Radiant Energy System (CERES) on the Tropical Rainfall Measuring Mission (TRMM), Terra, and Aqua satellites. The daytime method uses the 0.65-, 3.8-, 10.8-, and 12.0-mu m channels on the TRMM Visible and Infrared Scanner (VIRS) and the Terra and Aqua MODIS. The VIRS and Terra 1.6-mu m channel and the Aqua 1.38- and 2.1-mu m channels are used secondarily. The primary nighttime radiances are from the 3.8-, 10.8-, and 12.0-mu m channels. Significant differences were found between the VIRS and Terra 1.6-mu m and the Terra and Aqua 3.8-mu m channels' calibrations. Cascading threshold tests provide clear or cloudy classifications that are qualified according to confidence levels or other conditions, such as sunglint, that affect the classification. The initial infrared threshold test classifies similar to 43% of the pixels as clouds. The next level seeks consistency in three (two) different channels during daytime (nighttime) and accounts for roughly 40% (25%) of the pixels. The third tier uses refined thresholds to classify remaining pixels. For cloudy pixels, similar to 4% yield no retrieval when analyzed with a cloud retrieval algorithm. The techniques were applied to data between 1998 and 2006 to yield average nonpolar cloud amounts of similar to 0.60. Averages among the platforms differ by < 0.01 and are comparable to surface climatological values, but roughly 0.07 less than means from two other satellite analyses, primarily as a result of missing small subpixel and thin clouds.
引用
收藏
页码:3857 / 3884
页数:24
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