Ge. Flowers et Gkc. Clarke, Surface and bed topography of Trapridge Glacier, Yukon Territory, Canada: digital elevation models and derived hydraulic geometry, J GLACIOL, 45(149), 1999, pp. 165-174
Measurements of ice thickness and surface elevation are prerequisite to man
y glaciological investigations. A variety of techniques has been developed
for interpretation of these data, including means of constructing regularly
gridded digital elevation models (DEMs) for use in numerical studies. Here
we present a simple yet statistically sound method for processing ice-pene
trating radar data and describe a technique for interpolating these data on
to a regular grid. DEMs generated for Trapridge Glacier, Yukon Territory, C
anada, are used to derive geometric quantities that give preliminary insigh
ts into the underlying basin-scale hydrological system. This simple geometr
ic analysis suggests that at low water pressures a dendritic drainage netwo
rk exists that evolves into a uniaxial morphology as water pressure approac
hes flotation. These predictions are compared to hydraulic connection proba
bilities based on borehole drilling.