Validation of VEGETATION, MODIS, and GOES plus SSM/I snow-cover products over Canada based on surface snow depth observations

被引:153
作者
Simic, A
Fernandes, R
Brown, R
Romanov, P
Park, W
机构
[1] Canada Ctr Remote Sensing, Nat Resources Canada, Ottawa, ON K1A OY7, Canada
[2] Noetix Res Inc, Ottawa, ON, Canada
[3] Meteorol Serv Canada, Dorval, PQ, Canada
[4] NOAA, NESDIS, Off Res & Applicat, Camp Springs, MD USA
关键词
remote sensing; snow cover; MODIS; GOES; SSM/I; SPOT-VGT; validation;
D O I
10.1002/hyp.5509
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The ability to map the areal depletion of snow accurately is important for operational decision making (e.g. reservoir management), for correct specification of boundary conditions in numerical weather-prediction models, and for modelling atmospheric, hydrological and ecological processes. A number of satellite-derived snow-cover products are available in real time; however, these can differ considerably due to variations in sensor and platform characteristics, data pre-processing methods, and the particular snow-cover classification algorithms employed. This article evaluates the performance of three daily snow-cover products over Canada: (1) Terra Moderate Resolution Imaging Spectroradiometer (MODIS) snow-cover maps provided at 500 m spatial resolution for 2001; (2) National Oceanic Atmospheric Administration (NOAA) GOES + SSM/I snow maps provided at 4 km resolution for 2001 (similar to30 km resolution SSM/I data were used for cloud-covered areas); (3) SPOT-4 VEGETATION (VGT) snow maps derived at 1 km resolution for 2000. An evaluation of the snow-cover products with daily surface snow depth observations collected from almost 2000 meteorological stations across Canada revealed that the VGT snow product used in this study may not be suitable for snow mapping in Canada because of a significant bias towards mapping snow-free conditions. The MODIS and NOAA products showed similar reasonable levels of agreement with ground data, ranging from approximately 80% to 100% on a monthly basis. Somewhat lower agreement was found in January, when solar zenith angles are large, suggesting that better correction for tree and surface shadow effects is needed in current snow-cover mapping algorithms. The lowest agreement was seen during snowmelt, mainly in forest areas. Comparison of MODIS agreement statistics between sparse and dense conifer regions indicated that the effect of non-representativenes of surface snow depth observations was on the order of 10% disagreement. The NOAA product was found to be the most consistent among land cover types and had the highest percentage of cloud-free pixels. Copyright (C) 2004 John Wiley Sons, Ltd.
引用
收藏
页码:1089 / 1104
页数:16
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