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An Adaptive Neural Network System for Improving the Filtration of Non-Snow Pixels from SSM/I Images

机译:一种改进神经网络系统,用于改善SSM / I图像的非雪像素过滤

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Snow-cover parameters are being increasingly used as input to hydrological models. Having an accurate estimation of snow cover characteristics during the snowmelt season is indispensable for an efficient hydrological modeling and snowmelt runoff forecasting. Direct measurements of snow depth at a single station are generally not very useful in making estimates of distribution over large areas, since the measured depth may be highly unrepresentative of the neighboring area because of drifting or blowing. Additionally, the traditional field sampling methods and the ground-based data collection are often very sparse, time consuming, and expensive compared to the coverage provided by remote sensing techniques. At present, most of hydrological models that require snowpack information are using maps obtained by gridding standard point gauge measurements or derived from physicaily/statistically-based models. In this paper, we used an adaptive neural network system to generate the spatial distribution of snow accumulation from multi-channel SSM/I data in the Northern Midwest of the United States. Five SSM/I channels were used in this experiment (19H, 19V, 22V, 37V, and 85V). Three snow days with high snow accumulation and no precipitation have been selected during the 2001/2002 winter season. Snow depth measurements have been collected from the National Climatic Data Center (NCDC) through the Cooperative Observer Network for the U.S. snow Monitoring. The snow depths have been compiled and gridded into 25 km × 25 km grid to match the final SSM/I resolution.
机译:雪覆盖参数越来越多地用作水文模型的输入。在散雪季节期间对雪覆盖特性进行了准确估计,对于有效的水文建模和雪花径流预测是不可或缺的。在单个站的直接测量在单个站中的雪深度通常在大面积上进行分布估计,因此由于漂移或吹气,测量的深度可能是高度不合格的相邻区域。另外,与通过遥感技术提供的覆盖范围相比,传统的现场采样方法和地基数据收集通常非常稀疏,耗时且昂贵。目前,需要SnowPack信息的大多数水文模型都使用通过网格标准点仪表测量而获得的映射或从基于物理/统计学的模型衍生。在本文中,我们使用了自适应神经网络系统,从美国北部的北部的多通道SSM / I数据产生了积雪的空间分布。在本实验(19h,19V,22V,37V和85V)中使用了五个SSM / I频道。在2001/2002年冬季,已经选择了高积雪累积和没有降水的三个雪天。已经通过国家气候数据中心(NCDC)收集了雪深度测量,通过了美国雪监测的合作观察网络。雪深层已编译并将其包装成25公里×25 km网格,以匹配最终的SSM / I分辨率。

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