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Calculating terrain indices along streams: A new method for separating stream sides

机译:计算河流的地形指数:一种分离河流两侧的新方法

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摘要

There is increasing interest in assessing riparian zones and their hydrological and biogeochemical buffering capacity with indices derived from hydrologic landscape analysis of digital elevation data. Upslope contributing area is a common surrogate for lateral water flows and can be used to assess the variability of local water inflows to riparian zones and streams. However, current geographic information system algorithms do not provide a method for easily separating riparian zone and adjacent upland lateral contributions on each side of the stream. Here we propose a new algorithm to compute side-separated contributions along stream networks. We describe the new algorithm and illustrate the importance of distinguishing between lateral inflows on each side of streams with hillslope-riparian zone-stream hydrologic connectivity results from high-frequency water table data collected in the 22 km~2 Tenderfoot Creek catchment, Montana.
机译:人们对利用来自数字高程数据的水文景观分析得出的指标来评估河岸带及其水文和生物地球化学缓冲能力的兴趣日益浓厚。上坡贡献区是横向水流的常见替代物,可用于评估局部水流入河岸带和河流的变化性。然而,当前的地理信息系统算法没有提供一种用于容易地分离河流的每一侧上的河岸带和相邻的高地横向贡献的方法。在这里,我们提出了一种新的算法来计算沿流网络的边分离贡献。我们描述了该新算法,并说明了在蒙大拿州22 km〜2 Tenderfoot Creek流域收集的高频地下水位数据与山坡—河岸带—水文水文连通性结果之间,区分溪流两侧的横向流入的重要性。

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  • 来源
    《Water resources research》 |2010年第12期|p.W12536.1-W12536.10|共10页
  • 作者单位

    Department of Physical Geography and Quaternary Geology. Stockholm University. Stockholm. Sweden;

    Department of Land Resources and Environmental Sciences. Montana State University. Bozeman. Montana, USA;

    Department of Land Resources and Environmental Sciences. Montana State University. Bozeman. Montana, USA;

    Department of Physical Geography and Quaternary Geology. Stockholm University. Stockholm. Sweden,Department of Geography. University of Zurich. Zurich. Switzerland;

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  • 正文语种 eng
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  • 入库时间 2022-08-18 03:39:06

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