Controls on runoff from a partially harvested aspen-forested headwater catchment, Boreal Plain, Canada
Version of Record online: 13 JAN 2005
Copyright © 2005 John Wiley & Sons, Ltd.
Special Issue: Canadian Geophysical Union—Hydrology Section
Volume 19, Issue 1, pages 3–25, January 2005
How to Cite
Devito, K. J., Creed, I. F. and Fraser, C. J. D. (2005), Controls on runoff from a partially harvested aspen-forested headwater catchment, Boreal Plain, Canada. Hydrol. Process., 19: 3–25. doi: 10.1002/hyp.5776
- Issue online: 13 JAN 2005
- Version of Record online: 13 JAN 2005
- Manuscript Accepted: 1 MAR 2004
- Manuscript Received: 23 JUN 2003
- Alberta Pacific Forestry Industries Inc.
- aspen forest;
- Boreal Plain;
- forest harvest;
- soil storage;
- surface saturation;
- water balance
The water balance and runoff regime of a 55 ha aspen-forested headwater catchment located on the Boreal Plain, Alberta, Canada (55·1°N, 113·8°W) were determined for 5 years following a partial timber harvest. Variability in precipitation provided the opportunity to contrast catchment water balances in relatively dry (<350 mm year−1), wet (>500 mm year−1), and average precipitation years. In most years, the catchment water balance was dominated by soil water storage, evapotranspiration losses, and vertical recharge. In 1997, despite near-average annual precipitation (486 mm), there was significant runoff (250 mm year−1) with a runoff coefficient of 52%. A wet summer and autumn in the preceding year (1996) and large snow accumulation in the spring (1997) reduced the soil water storage potential, and large runoff occurred in response to a substantial July rainfall event. Maps of the surface saturated areas indicated that runoff was generated from the uplands, ephemeral draws, and valley-bottom wetlands. Following 1997, evapotranspiration exceeded precipitation and large soil water storage potentials developed, resulting in a reduction in surface runoff to 11 mm in 1998, and <2 mm in 1999–2001. During this time, the uplands were hydrologically disconnected from ephemeral draws and valley-bottom wetlands. Interannual variability was influenced by the degree of saturation and connectivity of ephemeral draws and valley wetlands. Variability in runoff from tributaries within the catchment was influenced by the soil water storage capacity as defined by the depth to the confining layer. An analysis of the regional water balance over the past 30 years indicated that the potential to exceed upland soil water storage capacity, to connect uplands to low-lying areas, and to generate significant runoff may only occur about once every 20 years. The spatial and temporal variability of soil water storage capacity in relation to evaporation and precipitation deficits complicates interpretation of forest harvesting studies, and low runoff responses may mask the impacts of harvesting of aspen headwater areas on surface runoff in subhumid climates of the Boreal Plain. Copyright © 2005 John Wiley & Sons, Ltd.