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Hibbert Hibbert (1983)
Water yield improvement potential by vegetation management on western rangelandsWater Resour. Bull., 19
Harr Harr (1983)
Potential for augmenting water yield through forest practices in western Washington and western OregonWater Resour. Bull., 19
H. Wilm, E. Dunford (1948)
Effect of Timber Cutting on Water Available for Stream Flow from a Lodgepole Pine Forest
J. Bosch, J. Hewlett (1982)
A REVIEW OF CATCHMENT EXPERIMENTS TO DETERMINE THE EFFECT OF VEGETATION CHANGES ON WATER YIELD AND EVAPOTRANSPIRATIONJournal of Hydrology, 55
J. Douglass (1983)
THE POTENTIAL FOR WATER YIELD AUGMENTATION FROM FOREST MANAGEMENT IN THE EASTERN UNITED STATES1Journal of The American Water Resources Association, 19
(1959)
Management of forest stands in western United States to influence the. flow of snow-fed streams
R. Kattelmann, N. Berg, J. Rector (1983)
THE POTENTIAL FOR INCREASING STREAMFLOW FROM SIERRA NEVADA WATERSHEDSJournal of The American Water Resources Association, 19
H. Gisborne (1942)
Results and trends at the Northern Rocky Mountain Forest and Range Experiment Station, 16
Kattelmann Kattelmann, Berg Berg, Rector Rector (1983)
The potential for increasing streamflow from Sierra Nevada watershedsWater Resour. Bull., 19
(1981)
Wagon Wheel Gap watershed experiment revisited
Troendle Troendle (1983)
The potential for water yield augmentation from forest management in the Rocky Mountain regionWater Resour. Bull., 19
R. Harr (1983)
POTENTIAL FOR AUGMENTING WATER YIELD THROUGH FOREST PRACTICES IN WESTERN WASHINGTON AND WESTERN OREGONJournal of The American Water Resources Association, 19
C. Troendle (1983)
The Potential for Water Yield Augmentation from Forest Management in the Rocky Mountain RegionJournal of The American Water Resources Association, 19
(1967)
Process and significance of interception in Colorado subalpine forest
A. Hibbert (1983)
Water Yield Improvement Potential by Vegetation Management on Western RangelandsJournal of The American Water Resources Association, 19
C. Leaf (1975)
Watershed management in the Rocky Mountain subalpine zone: the status of our knowledge
(1984)
Options for harvesting timber to control snowpack accumulations
(1981)
Effects of timber harvest in the snow zone on volume and timing of water yield, in Interior West Watershed management
(1985)
Snowpack accumulation before and after thinning a dog-hair stand of lodgepole pine
(1980)
An approach to water resources evaluation of non-point silvicultural sources
C. Leaf, J. Kovner (1972)
Sampling requirements for areal water equivalent estimates in forested subalpine watershedsWater Resources Research, 8
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Vegetation management for water yield, in Water Balance in North America, pp. 191-195
M. Kaufmann (1985)
Modelling transpiration of subalpine trees in the central Rocky Mountains
The Fool Creek watershed at the Fraser Experimental Forest, Colorado was harvested using a pattern of alternating clearcut and forested strips in 1956. Today, with almost 30 years of postharvest record, subtle impacts on the hydrology of the watershed can be detected that were not significant in the past. In addition to the depositional increases in the snowpack in the openings, average peak water equivalent over the entire watershed has been increased (9%). Long‐term, postharvest, climatic records now available show a strong correlation between estimated increases in flow and winter and melt period precipitation. Much of the annual variability in increased flow, now explained by precipitation, was formerly attributed to regrowth or time. Peak discharges, advanced 7.5 days following harvest, have also been increased 20%, with the largest effect occurring in the wettest years. Increases in peak water equivalent, annual flow, and date of peak flow occurrence all appear to be returning to preharvest levels at a very slow rate.
Water Resources Research – Wiley
Published: Dec 1, 1985
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