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Estimation of snow depth over open prairie environments using GOES imager observations

机译:使用GOES成像仪观测估算开阔大草原环境下的积雪深度

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We assess the potential for estimating snow depth using observations in the visible and infrared spectral bands from the imager instrument onboard the Geostationary Operational Environmental Satellites (GOES). The approach makes use of a correlation between depth of the snowpack and satellite-derived subpixel fractional snow cover over non-forested and sparsely forested areas. To retrieve the snow depth we propose a simple analytical formula approximating the statistical relationship between the snow depth and the snow fraction. The primary focus of this study was the US Great Plains and Canadian prairies area. Daily maps of snow depth at a spatial resolution of 4 km have been produced for this region for four winter seasons from late 1999 to the beginning of 2003. Validation of the algorithm developed was performed through comparison of the satellite-based product with snow depth measurements made at first-order synoptic stations, US Cooperative Network stations and Canadian climate stations. The accuracy of snow depth retrievals was found to be about 30% of the observed snow depth for snow depths below 30 cm.
机译:我们使用对地静止作战环境卫星(GOES)上成像仪的可见光谱和红外光谱带中的观测值来评估估计雪深的潜力。该方法利用了积雪的深度与非森林和稀疏森林区域上的卫星衍生的亚像素分数积雪之间的相关性。为了检索积雪深度,我们提出了一个简单的解析公式,用于近似化积雪深度和积雪分数之间的统计关系。这项研究的主要重点是美国大平原和加拿大大草原地区。从1999年下半年到2003年初的四个冬季,该地区的日积雪深度分辨率为4 km,已绘制出每日地图。通过对基于卫星的产品与积雪深度测量值进行比较,对开发的算法进行了验证。在一级天气站,美国合作网络站和加拿大气候站生产。对于30厘米以下的积雪深度,发现积雪深度的准确性约为观测积雪深度的30%。

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