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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Validation of daily MODIS snow cover maps of the Upper Rio Grande River Basin for the 2000-2001 snow year
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Validation of daily MODIS snow cover maps of the Upper Rio Grande River Basin for the 2000-2001 snow year

机译:验证2000-2001雪年上里约格兰德河上游的每日MODIS雪盖图

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Snow cover represents an important water resource for the Upper Rio Grande River Basin of Colorado and New Mexico. Accuracy assessment of MODIS snow products was accomplished using Geographic Information System (GIS) techniques. Daily snow cover maps produced from Moderate Resolution Imaging Spectroradiometer (MODIS) data were compared with operational snow cover maps produced by the National Operational Hydrologic Remote Sensing Center (NOHRSC) and against in situ Snowpack Telemetry (SNOTEL) measurements for the 2000-2001 snow season. Over the snow season, agreement between the MODIS and NOHRSC snow maps was high with an overall agreement of 86%. However, MODIS snow maps typically indicate a higher proportion of the basin as being snow-covered than do the NOHRSC snow maps. In particular, large tracts of evergreen forest on the western slopes of the San de Cristo Range, which comprise a large portion of the eastern margin of the basin, are more consistently mapped as snow-covered in the MODIS snow products than in the NOHRSC snow products. NOHRSC snow maps, however, typically indicate a greater proportion of the central portion of the basin, predominately in cultivated areas, as snow. Comparisons of both snow maps with in situ SNOTEL measurements over the snow season show good overall agreement with overall accuracies of 94% and 76% for MODIS and NOHRSC, respectively. A lengthened comparison of MODIS against SNOTEL sites, which increases the number of comparisons of snow-free conditions, indicates a slightly lower overall classification accuracy of 88%. Errors in mapping extra snow and missing snow by MODIS are comparable, with MODIS missing snow in approximately 12% of the cases and mapping too much snow in 15% of the cases. The majority of the days when MODIS fails to map snow occurs at snow depths of less than 4 cm. (C) 2003 Elsevier Science Inc. All rights reserved. [References: 25]
机译:积雪是科罗拉多州和新墨西哥州上里奥格兰德河流域的重要水资源。 MODIS雪产品的准确性评估是使用地理信息系统(GIS)技术完成的。将中分辨率成像光谱仪(MODIS)数据产生的每日积雪图与国家运行水文遥感中心(NOHRSC)产生的积雪图进行比较,并与2000-2001年雪季的原地积雪遥测(SNOTEL)测量进行比较。在积雪季节,MODIS和NOHRSC积雪图之间的一致性很高,总体一致性为86%。但是,与NOHRSC的雪图相比,MODIS的雪图通常表示该盆地被雪覆盖的比例更高。特别是,圣克里斯托山脉西部斜坡上的大片常绿森林(占盆地东缘的大部分)被映射为MODIS雪产品中的积雪比NOHRSC雪中的雪更一致产品。但是,NORHRC的积雪图通常表示流域中部的比例较大,主要是在耕种区,如积雪。两种雪图与雪季原位SNOTEL测量值的比较显示出良好的总体一致性,MODIS和NOHRSC的总体准确度分别为94%和76%。与SNOTEL站点进行MODIS的较长的比较,这增加了无雪条件的比较次数,这表明整体分类精度略低,为88%。 MODIS映射多余积雪和失雪的错误是可比的,在大约12%的案例中MODIS失雪并且在15%的案例中映射过多的雪。 MODIS无法绘制积雪的大部分日子都发生在积雪深度小于4厘米的地方。 (C)2003 Elsevier Science Inc.保留所有权利。 [参考:25]

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