Evaluation of the MODIS snow cover fraction product

被引:55
作者
Arsenault, Kristi R. [1 ,2 ]
Houser, Paul R. [3 ]
De Lannoy, Gabrielle J. M. [2 ,4 ]
机构
[1] Sci Applicat Int Corp, Beltsville, MD USA
[2] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[3] George Mason Univ, Fairfax, VA 22030 USA
[4] Univ Ghent, B-9000 Ghent, Belgium
关键词
snow cover fraction; remote sensing; land surface modeling; WATER EQUIVALENT; RIVER-BASIN; NORTHERN XINJIANG; CLOUD MASK; VALIDATION; ACCURACY; RESOLUTION; MAPS; COMBINATION; VEGETATION;
D O I
10.1002/hyp.9636
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Eleven years of daily 500m gridded Terra Moderate Resolution Imaging Spectroradiometer (MODIS) (MOD10A1) snow cover fraction (SCF) data are evaluated in terms of snow presence detection in Colorado and Washington states. The SCF detection validation study is performed using in-situ measurements and expressed in terms of snow and land detection and misclassification frequencies. A major aspect addressed in this study involves the shifting of pixel values in time due to sensor viewing angles and gridding artifacts of MODIS sensor products. To account for this error, 500m gridded pixels are grouped and aggregated to different-sized areas to incorporate neighboring pixel information. With pixel aggregation, both the probability of detection (POD) and the false alarm ratios increase for almost all cases. Of the false negative (FN) and false positive values (referred to as the total error when combined), FN estimates dominate most of the total error and are greatly reduced with aggregation. The greatest POD increases and total error reductions occur with going from a single 500m pixel to 3x3-pixel averaged areas. Since the MODIS SCF algorithm was developed under ideal conditions, SCF detection is also evaluated for varying conditions of vegetation, elevation, cloud cover and air temperature. Finally, using a direct insertion data assimilation approach, pixel averaged MODIS SCF observations are shown to improve modeled snowpack conditions over the single pixel observations due to the smoothing of more error-prone observations and more accurately snow-classified pixels. Copyright (c) 2012 John Wiley & Sons, Ltd.
引用
收藏
页码:980 / 998
页数:19
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