首页> 外文会议>第21届国际摄影测量与遥感大会(ISPRS 2008)论文集 >DERIVING LAND USE AND CANOPY COVER FACTOR FROM REMOTE SENSING AND FIELD DATA IN INACCESSIBLE MOUNTAINOUS TERRAIN FOR USE IN SOIL EROSION MODELLING
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DERIVING LAND USE AND CANOPY COVER FACTOR FROM REMOTE SENSING AND FIELD DATA IN INACCESSIBLE MOUNTAINOUS TERRAIN FOR USE IN SOIL EROSION MODELLING

机译:从无法遥感的山地土壤遥感数据和田间数据中推导土地利用和冠层覆盖因子,以用于土壤侵蚀模型

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Soil erosion is one of the severe land degradation problems in many parts of the world. It not only affects on decreasing agricultural productivity but also it causes disasters such as siltation of reservoirs and flooding in low lying areas in case of high rainfall events. To predict soil losses various models are available the results of which can be used for formulating soil conservation planning. In order to run the predictive models, one of the crucial data required is the land cover/land use and the canopy cover information. While land cover data can be used to derive information on effective soil hydrological depths and to estimate kinetic energy of leaf drainage, vegetation canopy cover will give information on rain interception factor, both of which are important input in calculating runoff and soil loss. These data may not be easily available in many mountainous areas because of inaccessibility problem. In this situation remote sensing data becomes very important. For classification of remote sensing data, however, one has to keep into account the problem due to illumination variations induced by variations in topography in mountainous areas, which may not lead to normal distribution of training samples, an assumption required by maximum likelihood classification. To solve this problem, illumination variation was removed using different techniques. The resulting data was classified to generate land use map. The result shows improvement in classification accuracy. The cover factor or the C factor is generally estimated using normalized difference vegetation index (NDVI) assuming a linear relationship which may not be the case always. The surface cover includes not only vegetation canopy cover but also plant residue and soil surface cover. In this study C-factor is derived by using in first place field assessment and then followed by calculating normalized difference vegetation index (NDVI). Correlation is carried out and a curve is fitted. The estimated C-factor represents the percent ground cover for each land cover type, as well as the presence of plant residue. The result was tested for its reliability and estimation error using field data, which shows that the coefficient of efficiency was higher (0.77) and the root mean square error was 0.03. The study was applied in a watershed in northern Thailand
机译:在世界许多地方,水土流失是严重的土地退化问题之一。它不仅影响农业生产率的下降,而且还会在高降雨事件下造成诸如水库淤积和低洼地区洪水之类的灾难。为了预测水土流失,可以使用各种模型,其结果可用于制定水土保持计划。为了运行预测模型,所需的关键数据之一是土地覆盖/土地利用和冠层覆盖信息。虽然土地覆盖数据可用于得出有关有效土壤水文深度的信息并估算叶片排水的动能,但植被冠层覆盖将提供有关降雨截留因子的信息,这两者都是计算径流和土壤流失的重要输入。由于无法访问的问题,在许多山区可能无法轻易获得这些数据。在这种情况下,遥感数据变得非常重要。然而,对于遥感数据的分类,必须考虑到由山区地形变化引起的照明变化引起的问题,这可能不会导致训练样本的正态分布,这是最大似然分类所要求的。为了解决这个问题,使用不同的技术消除了照明变化。对所得数据进行分类以生成土地使用图。结果显示了分类准确性的提高。覆盖因子或C因子通常使用归一化植被指数(NDVI)进行估算,并假设并非总是线性关系。地表覆盖物不仅包括植被冠层覆盖物,还包括植物残渣和土壤表面覆盖物。在这项研究中,首先通过现场评估得出C因子,然后再计算归一化差异植被指数(NDVI)。进行相关并拟合曲线。估计的C因子代表每种土地覆被类型的地面覆被百分比,以及植物残存物的存在。使用现场数据测试了结果的可靠性和估计误差,结果表明效率系数更高(0.77),均方根误差为0.03。该研究被应用于泰国北部的一个分水岭

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