In many spatial analyses and GIS applications, a Digital Elevation Model (D
EM) is often used to derive a variety of new variables and parameters. Prev
ious research shows that the accuracy of derived variables is affected, not
merely by the magnitude of DEM errors and the algorithms applied to derive
these variables, but also by the spatial structure of DEM errors. However;
the back of knowledge and understanding of the spatial structure of DEM er
rors often handicaps the analysis of error propagation.
This paper investigates the spatial autocorrelation and anisotropic pattern
of DEM error by using directional variograms in the spatial domain and Fou
rier analysis in the frequency domain. Based on an empirical study, it is c
oncluded that the spatial autocorrelation pattern of DEM errors is anisotro
pic and scale-dependent, and that the maximum direction and range of the au
tocorrelation depends upon the orientation and wavelength of the terrain fe
atures. For a smooth terrain, the magnitude of DEM errors is correlated to
surface slope. For a rugged terrain, the elevation values in DEMs tend to b
e underestimated in ridges, and overestimated in valleys, but the correlati
on between the DEM error and surface slope is quits low.