CGRG Bibliography of Canadian Geomorphology
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Author : Bauch, G.D.; and Hickin, E.J.
Date : 2007.
Title : Flooding rains and river change: 50 years of hydrogeomorphology of Squamish River, southwestern British Columbia.
Publication : CANQUA Ottawa 2007. Canadian Quaternary Association Conference, June 4-8, 2007. Carleton University, Ottawa, Ontario, Canada.
Issue :
Page(s) :
Abstract
Squamish River basin in SW coastal British Columbia is an important catchment in which a series of scientific studies of fluvial geomorphology, sedimentology, and Quaternary science have been completed during the last several decades. Here we review a half-century record (1956-2005) of daily discharge of Squamish River (at Brackendale) to evaluate hydrologic trends.Although the mean discharge series is stationary, that for large floods (>1500m3s-1) is strongly upward trending over time. This trend to increased extreme flooding appears to be driven by intensifying fall/winter storms that have increased rainfall intensity and storm duration. There is no evidence to suggest that endogenous hydrologic shifts related to landuse change are a significant factor. Channel changes have been documented elsewhere for Squamish River for the period 1947-1984; it is expected that the pattern of channel change has intensified over the last two decades. Investigation of this expectation is the subject of ongoing research at Simon Fraser University.
Bibliography of Canadian Geomorphology