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Examining development-induced geomorphic change using multi-temporal LiDAR-derived digital elevation models.

机译:使用多时间LiDAR衍生的数字高程模型检查由开发引起的地貌变化。

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摘要

During development, topography is cut, filled, and graded, altering natural surface drainage patterns. The spatiotemporal characteristics of drainage network and hillslope changes throughout the development process are to date unknown. For this study we used multiple temporal LiDAR-derived DEMs spanning the development of two small agricultural watersheds to examine geomorphic changes caused by urban development. A third forested watershed was also examined to track geomorphic changes not attributable to development. We first present a technique to extract drainage channel heads and drainage networks through time utilizing surface tangential curvature and compare its ability to predict field verified channel heads against two other delineation techniques. Second, subwatersheds of the delineated networks were used to summarize topographic changes in the forested and developing watersheds through time. Finally, simplified hydrologic response functions are generated for each time step utilizing width functions augmented by curvature delineated networks. Landscape dissection and hydrologic connectivity increased throughout development, indicating an increased efficiency of water removal from the landscape. Substantial topographic changes manifest as variations in curvature standard deviations through time in first order catchments, highlighting redistributions of high and low gradient regions. Idealized hydrologic responses reflect increased landscape connectivity with a distinct shift toward more rapid storm response shapes throughout the development process. Unexpectedly high temporal variance observed in the forested watershed across analyses indicates inherent differences in digital topographic datasets collected on different dates. Results of this thesis highlight fundamental geomorphic changes caused by development practices while developing methods and rationale for temporal DEM-based geomorphic studies.
机译:在开发过程中,地形被切割,填充和分级,从而改变了自然地表排水模式。迄今为止,在整个开发过程中,排水网络的时空特征和山坡变化都是未知的。在本研究中,我们使用跨越两个小型农业流域发展的多个时间LiDAR派生的DEM来研究由城市发展引起的地貌变化。还检查了第三个森林流域,以追踪与发展无关的地貌变化。我们首先提出一种利用表面切向曲率通过时间提取排水通道水头和排水网络的技术,并比较其预测场验证通道水头与其他两种轮廓技术的能力。其次,使用划定的网络的子集水区来总结森林和发展中集水区随时间的地形变化。最后,利用由曲率描述网络扩展的宽度函数为每个时间步生成简化的水文响应函数。在整个开发过程中,景观解剖和水文连通性增加,表明从景观中除水的效率提高。大量的地形变化表现为一阶流域的曲率标准偏差随时间的变化,突出了高和低梯度区域的重新分布。理想的水文响应反映了景观连通性的增强,并且在整个开发过程中都朝着更快的风暴响应形状明显转移。跨分析在森林流域中观察到的出乎意料的高时空变化表明在不同日期收集的数字地形数据集的固有差异。本文的结果强调了开发实践引起的基本地貌变化,同时为基于DEM的时间地貌研究开发了方法和原理。

著录项

  • 作者

    Jones, Daniel Kyle.;

  • 作者单位

    University of Maryland, Baltimore County.;

  • 授予单位 University of Maryland, Baltimore County.;
  • 学科 Geodesy.;Land Use Planning.;Geomorphology.
  • 学位 M.S.
  • 年度 2013
  • 页码 171 p.
  • 总页数 171
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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