刘学军, 张平. DEM坡度、坡向的有效尺度范围[J]. 武汉大学学报 ( 信息科学版), 2008, 33(12): 1254-1258.
引用本文: 刘学军, 张平. DEM坡度、坡向的有效尺度范围[J]. 武汉大学学报 ( 信息科学版), 2008, 33(12): 1254-1258.
LIU Xuejun, ZHANG Ping. Effective Scale of Slope and Aspect Derived from Grid-based Digital Elevation Model[J]. Geomatics and Information Science of Wuhan University, 2008, 33(12): 1254-1258.
Citation: LIU Xuejun, ZHANG Ping. Effective Scale of Slope and Aspect Derived from Grid-based Digital Elevation Model[J]. Geomatics and Information Science of Wuhan University, 2008, 33(12): 1254-1258.

DEM坡度、坡向的有效尺度范围

Effective Scale of Slope and Aspect Derived from Grid-based Digital Elevation Model

  • 摘要: 采用曲面矢量合成方法,通过比较点位上的坡度、坡向的矢量值与以点为中心、一定范围地形曲面上的矢量值,进行了DEM坡度、坡向的有效尺度范围研究。结果表明,格网中心点上计算得到的坡度、坡向所代表的范围是DEM分辨率的1.7~2.7倍。这种规律在不同的地貌样区是普遍存在的,且不受DEM分辨率的影响。

     

    Abstract: Terrain parameters,such as slope and aspect,are the most frequently surface geomorphic parameters in terrain analysis,hydrological modeling,environmental studies and other geosciences fields.Currently,these terrain parameters are often estimated by 3×3 local moving window at grid-based digital elevation model(DEM);and the estimated value is set to the centre cell in 3×3 window.In other words,the slope/aspect map derived from DEM is the same resolution as the DEM.There exists a question in this observation whether the resolution of slope/aspect map is the same as the DEM resolution or not? Based on the vector algebra and real DEM,it demonstrates that the slope/aspect estimated by 3×3 window is larger than a grid cell of DEM,which is 1.7 to 2.7 times of DEM resolution.

     

/

返回文章
返回