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首页> 外文期刊>Hydrological Processes >Validation of VEGETATION, MODIS, and GOES + SSM/I snow-cover products over Canada based on surface snow depth observations
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Validation of VEGETATION, MODIS, and GOES + SSM/I snow-cover products over Canada based on surface snow depth observations

机译:根据地面积雪深度观察,对加拿大的VEGETATION,MODIS和GOES + SSM / I积雪产品进行验证

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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 (~30 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.
机译:准确绘制雪域枯竭图的能力对于运营决策(例如水库管理),在数值天气预报模型中正确指定边界条件以及对大气,水文和生态过程进行建模至关重要。实时提供了许多卫星衍生的积雪产品;但是,由于传感器和平台特性,数据预处理方法以及所采用的特定积雪分类算法的差异,这些差异可能会很大。本文评估了加拿大境内三种日常积雪产品的性能:(1)2001年以500 m空间分辨率提供的Terra中分辨率成像光谱仪(MODIS)积雪地图; (2)2001年以4 km分辨率提供的国家海洋大气管理局(NOAA)GOES + SSM / I雪图(云覆盖区域使用了约30 km分辨率的SSM / I数据); (3)2000年以1 km分辨率得出的SPOT-4植被(VGT)雪图。利用从加拿大近2000个气象站收集的每日地面雪深观测资料对积雪产品进行评估,结果表明,这项研究可能不适合加拿大的积雪测绘,因为它对无积雪状况的测绘有很大的偏见。 MODIS和NOAA产品与地面数据显示出相似的合理协议水平,范围从每月大约80%到100%。一月份发现较低的一致性,当时太阳天顶角很大,这表明在当前的积雪制图算法中需要对树和表面阴影效应进行更好的校正。融雪期间达成的协议最低,主要是在森林地区。稀疏针叶树地区和稠密针叶树地区之间的MODIS一致性统计比较表明,表雪深度观测的非代表性影响约为10%的差异。发现NOAA产品在土地覆盖类型中最一致,并且无云像素的百分比最高。

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