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Spatial and temporal runoff response to snowmelt, and the influence of geomorphology in a headwater catchment, central eastern Cascades, Washington

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Title Spatial and temporal runoff response to snowmelt, and the influence of
geomorphology in a headwater catchment, central eastern Cascades,
Washington
Names Alley, David (creator)
Date Issued 2007-03-23 (iso8601)
Note Graduation date: 2007
Abstract This report presents a nested gauging study of streamflow variability from three
sub-catchments (150-200 ha in area) of the Burns Creek catchment (565 ha) in the Entiat
Experimental Forest of central Washington State. We test and reject the hypothesis that
headwater catchments of this size are composed of physically and chemically
homogenous sub-catchments with regard to the volume and timing of runoff generation.
Our methods included sub-catchment distributed accounting of precipitation and
snowmelt, nested gauging of flow, and electrical conductance measurement (EC) for
water years 2005 and 2006. Our results showed that temporal and spatial contributions to
streamflow varied widely among the sub-catchments. Over 50% of annual precipitation
accumulated within the headwaters of the catchment, yet the highest elevation subcatchment
dominated streamflow only during the immediate melt season. Baseflow was
otherwise maintained by discharge from the lowest elevation sub-catchment. Flow and
EC data suggested groundwater dominated streamflow response to rainfall and snowmelt.
Over 90% of stormflow in each of the monitored sub-catchments was comprised of preevent
water using the standard two-component hydrograph separation method. Annual
runoff ratios and pre-event water contributions to streamflow increased with increasing
basin area. Runoff ratios from the three sub-catchments and the headwater catchment as
a whole were more uniform over the much wetter 2006 water year
Genre Research Paper
Identifier http://hdl.handle.net/1957/11223

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