Dm. Wolock, EFFECTS OF SUBBASIN SIZE ON TOPOGRAPHIC CHARACTERISTICS AND SIMULATEDFLOW PATHS IN SLEEPERS RIVER WATERSHED, VERMONT, Water resources research, 31(8), 1995, pp. 1989-1997
The effects of subbasin size on topographic characteristics and simula
ted flow paths were determined for the 111.5-km(2) Sleepers River Rese
arch Watershed in Vermont using the watershed model TOPMODEL. Topograp
hy is parameterized in TOPMODEL as the spatial and statistical distrib
ution of the index ln (a/tan B), where In is the Napierian logarithm,
a is the upslope area per unit contour length, and tan B is the slope
gradient. The mean, variance, and skew of the ln (a/tan B) distributio
n were computed for several sets of nested subbasins (0.05 to 111.5 km
(2)) along streams in the watershed and used as input to TOPMODEL. In
general, the statistics of the ln (a/tan B) distribution and the simul
ated percentage of overland flow in total streamflow increased rapidly
for some nested subbasins and decreased rapidly for others as subbasi
n size increased from 0.05 to 1 km(2), generally increased up to a sub
basin size of 5 km(2), and remained relatively constant at a subbasin
size greater than 5 km(2). Differences in simulated flow paths among s
ubbasins of all sizes (0.05 to 111.5 km(2)) were caused by differences
in the statistics of the ln (a/tan B) distribution, not by difference
s in the explicit spatial arrangement of ln (a/tan B) values within th
e subbasins. Analysis of streamflow chemistry data from the Neversink
River watershed in southeastern New York supports the hypothesis that
subbasin size affects flow-path characteristics.