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Comparison of topographic and physiographic properties measured on the ground with those derived from digital elevation models

机译:比较地面上测得的地形和地貌特性与数字高程模型得出的那些特性

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With the widespread availability of digital elevation models (DEM) and regional surveys of soils, topographic and physiographic features of landscapes are now more easily characterized. Within southwestern Oregon 391 field plots were registered within a geographic information system (GIS) to digitized topographic and soils coverages and properties extracted from the digital coverages compared with those estimated in the field. The initial comparison showed major differences in estimates of aspect, slope, and maximum available soil water content (#theta#), although the location of plots showed general agreement with elevations recorded on the maps. To extrapolate climatic data and interpret hydrologic responses accurately, an automated search procedure was developed whereby the initial location of each plot was, if necessary, shifted within specified bounds to give closer agreement with field estimates of aspect, slope, and #theta#. Specifically, the search routine sequentially identifies the nearest 100 m-resolution cell within a search radius of 3 or 5 cells in which differences are within +-22.5 deg of aspect, +-20% of slope, and in closest agreement with field estimates of 0. The search procedure resulted in improved agreement with field estimates: r~2s = 0.82 for aspect, 0.56 for slope, 0.54 for #theta#. To obtain these improvements required that the initial plot locations be shifted, on the average, 289m within the 3-pixel search radius, and 435 m within the 5 pixel radius. With the terrain analysis procedures developed in this paper, it is possible to overcome many problems associated with registering the precise location of field plots upon digitized topographic and soil maps. The procedure is particularly appropriate in situations where the environmental regimes associated with a specified field location are to be extrapolated across landscapes. The approach also permits a wealth of historical survey plot data to be incorporated into a GIS format and to be spatially extended.
机译:随着数字高程模型(DEM)的广泛使用以及对土壤的区域调查,现在可以更轻松地表征景观的地形和地貌特征。在俄勒冈州西南部的391个田地中,已在地理信息系统(GIS)中进行了注册,以对数字化的地形和土壤覆盖率以及从数字覆盖率中提取的特性进行实地评估。初步比较显示,在坡度,坡度和最大可用土壤含水量(#theta#)的估算上存在主要差异,尽管样地的位置与地图上记录的海拔高度大致一致。为了外推气候数据并准确解释水文响应,开发了一种自动搜索程序,根据需要,可以将每个图的初始位置移至指定范围内,以与纵横比,坡度和#theta#的现场估算值更加一致。具体来说,搜索例程会依次识别3或5个像元的搜索半径内最接近的100 m分辨率像元,其中差异在纵横比的+ -22.5度,坡度的-20%以内,并且与0.搜索程序提高了与现场估算值的一致性:纵横比r〜2s = 0.82,斜率0.56,#theta#0.54。为了获得这些改进,要求将初始绘图位置平均偏移为3像素搜索半径内的289m和5像素半径内的435m。利用本文开发的地形分析程序,可以克服许多与在数字化地形图和土壤图上记录田地图的精确位置有关的问题。该程序特别适用于要在整个景观中外推与指定野外地点相关的环境状况的情况。该方法还允许将大量的历史调查地块数据合并到GIS格式中并进行空间扩展。

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