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Effects of DEM resolution on the WEPP runoff and erosion predictions: A case study of forest areas in northern Idaho.

机译:DEM分辨率对WEPP径流和侵蚀预测的影响:以爱达荷州北部森林地区为例。

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摘要

DEMs (digital elevation models) can be used in a GIS (geographic information system) to represent topography and extract terrain features. DEMs vary in resolution and accuracy by the production method. The most widely used DEMs are the publicly accessible USGS (U.S. Geological Survey) NED (National Elevation Dataset) DEMs at 30-m and 10-m resolutions. There are other sources of DEMs with different resolutions and qualities, such as LIDAR (LIght Detection and Ranging) DEMs and SRTM (Shuttle Radar Topography Mission) DEMs. DEMs with different resolutions and sources can generate varied topographic and hydrologic features, which may in turn affect the runoff and sediment yield predictions in soil erosion models, such as the WEPP (Water Erosion Prediction Project) model.;This research project studies the effects of DEM resolutions and sources on (1) deriving topographic and hydrologic attributes, and (2) predicting watershed hydrology and water erosion using WEPP v2005. For two small forest watersheds located on Moscow Mountain in northern Idaho, six DEMs were prepared: LIDAR 30-m, 10-m, and 4-m DEMs, NED 30-m, 10-m DEMs, and SRTM 30-m DEM. These DEMs were used to calculate topographic and hydrologic parameters that served as inputs in WEPP. The model results were then compared with the runoff and sediment yield data observed at the watershed outlets.;This study has found that DEMs with different resolutions and sources can generate varied watershed shapes and structures, extract different hillslope and channel lengths and gradients, and produce significantly different sediment yield predictions in WEPP. In general, as DEM resolution became finer, its accuracy was higher, the landscape was more precisely and accurately represented, and the sediment yield estimates approached closer to the observed values. Conversely, as DEM resolution became coarser, its accuracy was lower, and the sediment yield estimates departed from the observed values. The study has also found that LIDAR DEMs are potentially very useful tools for soil erosion modeling.
机译:可以在GIS(地理信息系统)中使用DEM(数字高程模型)来表示地形并提取地形特征。 DEM的分辨率和精度因生产方法而异。使用最广泛的DEM是分辨率为30-m和10-m的可公开访问的USGS(美国地质调查局)NED(国家海拔数据集)DEM。还有其他具有不同分辨率和质量的DEM,例如LIDAR(光检测和测距)DEM和SRTM(穿梭雷达地形任务)DEM。具有不同分辨率和来源的DEM可以生成各种地形和水文特征,进而可能影响土壤侵蚀模型(如WEPP(水蚀预测项目)模型)中的径流和沉积物产量预测。 DEM的决议和资料来源(1)使用WEPP v2005得出地形和水文属性,以及(2)预测流域水文和水蚀。对于位于爱达荷州北部莫斯科山上的两个小森林流域,准备了六个DEM:LIDAR 30-m,10-m和4-m DEM,NED 30-m,10-m DEM和SRTM 30-m DEM。这些DEM用于计算WEPP中用作输入的地形和水文参数。然后将模型结果与在分水岭出口处观测到的径流和沉积物产量数据进行比较;该研究发现,具有不同分辨率和来源的DEM可以生成不同的分水岭形状和结构,提取不同的山坡和河道长度和坡度,并产生WEPP中的沉积物产量预测有显着差异。通常,随着DEM分辨率的提高,其精度更高,景观更精确,更准确,并且沉积物产量估算值越来越接近观测值。相反,随着DEM分辨率变粗,其精度会降低,并且沉积物产量估算值会偏离观测值。该研究还发现,激光雷达DEM是潜在的非常有用的土壤侵蚀建模工具。

著录项

  • 作者

    Zhang, Xinxin (Jane).;

  • 作者单位

    University of Idaho.;

  • 授予单位 University of Idaho.;
  • 学科 Geography.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 103 p.
  • 总页数 103
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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