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Operational snow cover estimation at subpixel scale using NOAA-AVHRR data

机译:使用NOAA-AVHRR数据进行亚像素规模的可操作积雪估算

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摘要

Snow and ice play an important role in the earth's radiation balance because of the high albedo in comparison to other natural surfaces. Furthermore ice and snow is the largest contributor to rivers and ground water over major parts of the middle and high altitudes. These are reasons why hydrological and climatological studies require estimates of snow covered areas. Most of such snow cover maps generated from satellite data include information of snow or not snow for each image pixel. In this study a linear spectral unmixing algorithm is used to calculate snow cover portions within each data cell. We examine the ability of this algorithm for operational and near-real time snow cover estimation at subpixel scale using medium spatial resolution satellite data from NOAA-AVHRR. The automated methodology is presented which produces snow cover fraction maps showing plausible distribution of snow in comparison to TERRA-ASTER data. The qualitative analysis of the results present how suitable the approach implemented in the preliminary processing chain is. Simplifying assumptions are made to the procedure which explains some variation between derived snow cover fraction map and reference data. Further work should include an accurate quantification of areal snow coverage comparison to traditional approaches.
机译:雪和冰在地球的辐射平衡中起着重要作用,因为与其他自然表面相比,反照率很高。此外,冰雪是中高海拔主要地区河流和地下水的最大贡献者。这就是为什么水文和气候学研究需要估计积雪面积的原因。从卫星数据生成的大多数这样的积雪图包括针对每个图像像素的降雪或不降雪的信息。在这项研究中,线性光谱分解算法用于计算每个数据单元中的积雪部分。我们使用来自NOAA-AVHRR的中等空间分辨率卫星数据,研究了该算法在亚像素尺度上进行操作和近实时雪盖估计的能力。提出了自动化的方法,该方法可以生成积雪覆盖图,与TERRA-ASTER数据相比,显示积雪的合理分布。对结果的定性分析显示了在初步处理链中实施的方法是否合适。对该过程进行了简化假设,该过程解释了得出的积雪覆盖图和参考数据之间的某些差异。进一步的工作应包括与传统方法相比,准确量化区域降雪覆盖率。

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