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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Channel head location and characteristics using digital elevation models
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Channel head location and characteristics using digital elevation models

机译:使用数字高程模型的通道头位置和特征

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The drainage network is the conduit through which much surface water and sediment are routed within a catchment. In a catchment, the position of where hillslopes begin and channels end has long been considered the position of transition between diffusive processes upslope and the more incisive fluvial processes downslope. Consequently, understanding channel head location is an important issue in understanding catchment hydrology and geomorphology. This study examines channel head position and characteristics in a catchment in Arnhem Land, Northern Territory, Australia. In this study the position of channel heads was mapped within the catchment and plotted on a reliable digital elevation model of the catchment. It was found that the majority of channel heads have relatively small source areas and that graphical catchment descriptors, such as the area-slope relationship and cumulative area distribution, can provide reliable measures of the field position of the heads of first-order streams and the transition from hillslope to channel. The area-slope relationship and cumulative area distribution are also shown to be good tools for determining digital elevation model grid size which can capture hillslope detail and the transition from hillslope to channel. Copyright (c) 2005 John Wiley & Sons, Ltd.
机译:排水网是集水区中大量地表水和沉积物通过其输送的管道。在一个流域中,长期以来一直认为山坡开始和河道结束的位置是扩散过程上坡与较尖锐的河流过程下坡之间的过渡位置。因此,了解河道水头位置是了解流域水文和地貌的重要问题。这项研究研究了澳大利亚北领地阿纳姆地的一个流域内河道的头部位置和特征。在这项研究中,在流域内绘制水头的位置,并绘制在流域可靠的数字高程模型上。已经发现,大多数通道头的源头面积相对较小,而图​​形集水量描述子(例如面积-坡度关系和累积面积分布)可以为一阶流头和水头的场位置提供可靠的度量。从山坡过渡到河道。面积-坡度关系和累积面积分布也被证明是确定数字高程模型网格大小的良好工具,可以捕获坡度细节以及从坡度到河道的过渡。版权所有(c)2005 John Wiley&Sons,Ltd.

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