Water Stewardship Information Sources

Citation Beckers J. and Y. Alila (2004). A model of rapid preferential hillslope runoff contributions to peak flow generation in a temperate rain forest watershed American Geophysical Union Water Resources Research, Vol. 40, No. 3, W03501. 10.1029/2003WR002582
Organization UBC
URL http://onlinelibrary.wiley.com/store/10.1029/2003WR002582/asset/wrcr9807.pdf?v=1&t=ihcw22i0&s=f74edb445ad92cb4754092109edebff2d8eccb63
Abstract/Description or Keywords A model for the 10 km2 Carnation Creek watershed on Vancouver Island, British
Columbia, is used to assess preferential hillslope runoff contributions to peak flow
generation. The model combines the matrix flow algorithm of the distributed hydrology
soil vegetation model with a Green-Ampt formulation for calculating matrix and by-pass
infiltration, preferential hillslope runoff initiation controlled by rainfall depth, and
downslope subsurface flow rates prescribed based on at-site tracer tests. Model evaluation
using 1972–1990 hydrometeorological data reveals that this formulation is successful
in simulating subannual and larger peak flows. Model results suggest that preferential flow
contributions to streamflow generation become greater than matrix flow contributions for
unit area discharge values in excess of 2.8 mm/hr, corresponding to a peak flow return
period of 2–3 months. This transition from matrix flow dominated runoff to preferential
flow dominated runoff is consistent with an observed upper limit of groundwater response
to precipitation for return periods in excess of 2 months. A break in slope in peak
flow frequency curves at a return period of about 20 months appears to correspond to a
change in storm characteristics. Thus at least three physically distinct populations of peak
flows may exist at Carnation Creek. The ability of the model to simulate peak flows
and groundwater responses for small and large storms suggests that it may be useful for
addressing runoff process considerations in the debate whether forest management
effects for annual and larger peak flows are similar to those inferred from analyses
dominated by subannual peak flows. INDEX TERMS: 1829 Hydrology: Groundwater hydrology;
1860 Hydrology: Runoff and streamflow; 1803 Hydrology: Anthropogenic effects; KEYWORDS: Watershed
hydrology, hillslope runoff, peak flows, preferential flow, DHSVM, British Columbia
Information Type article
Regional Watershed Vancouver Island South
Sub-watershed if known
Aquifer #
Comments
Project status complete
Contact Name Younes Alila
Contact Email [email protected]