Aw. Bingham et Wg. Rees, Construction of a high-resolution DEM of an Arctic ice cap using shape-from-shading, INT J REMOT, 20(15-16), 1999, pp. 3231-3242
Digital elevation models (DEMs) of ice sheets and ice caps are usually cons
tructed from elevation data acquired from airborne or satellite-borne altim
etric systems. Consequently, the DEMs have a spatial resolution of about 1
km which limits their use for most glaciological and remote sensing studies
. In this paper we investigated the possibility of using a shape-from-shadi
ng technique, applied to a Landsat MSS image, to create a high spatial reso
lution DEM of Austfonna, an ice cap in Svalbard. A high correlation (coeffi
cient of determination = 0.85) was observed between Landsat pixel brightnes
s values, acquired during winter, and the surface slope component parallel
to the solar azimuth. This relationship was used to create a DEM by calcula
ting surface elevation profiles across the ice cap, using low spatial resol
ution radio echo sounding data as tie points. The resulting DEM had an esti
mated rms error of about 14 m, with the error occurring mostly at low spati
al frequencies. Shape-from-shading produces less accurate DEMs than interfe
rometric SAR (InSAR) techniques. Nevertheless, in scenarios for which InSAR
cannot be used to construct a DEM, shape-from-shading provides an acceptab
le alternative.