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Harr Harr (1981)
Some characteristics and consequences of melt from shallow snowpacks during rainfall in western OregonJ. Hydrol., 53
(1973)
Dyrness, Natural vegetation of Oregon and Washington, U.S
(1975)
Experimental Forest, western Cascades, Oregon, U.S
Cheng (1975)
The evaluation of initial changes in peak streamflow following logging of a watershed on the west coast of CanadaIAHS-AISH Publ., 117
R. Harr (1977)
Water flux in soil and subsoil on a steep forested slopeJournal of Hydrology, 33
J. Hornbeck (1973)
Storm flow from hardwood‐forested and cleared watersheds in New HampshireWater Resources Research, 9
(1967)
Forest treatment effects on water
R. Harr, F. McCorison (1979)
Initial effects of clearcut logging on size and timing of peak flows in a small watershed in western OregonWater Resources Research, 15
J. Hewlett, J. Helvey (1970)
Effects of Forest Clear‐Felling on the Storm HydrographWater Resources Research, 6
(1969)
Hydrologic properties of soils on three small watersheds in the western Cascades of Oregon, U.S
R. Harr (1981)
Some characteristics and consequences of snowmelt during rainfall in western OregonJournal of Hydrology, 53
J. Rothacher, Pacific Forest, R. Station (1973)
Does harvest in west slope Douglas-fir increase peak flow in small forest streams?
W. Dixon, F. Massey (1951)
Introduction to Statistical Analysis
D. Harris (1973)
Hydrologic changes after clear-cut logging in a small Oregon coastal watershedJournal research U. S. geological survey, 1
J. Rothacher (1970)
Increases in Water Yield Following Clear‐Cut Logging in the Pacific NorthwestWater Resources Research, 6
R. Harr, W. Harper, James Krygier, F. Hsieh (1975)
Changes in storm hydrographs after road building and clear‐cutting in the Oregon Coast RangeWater Resources Research, 11
(1969)
Hydrologic properties of soils on three small watersheds in the western Cascades of Oregon , U . S . Dep
Timber harvest in two small watersheds in western Oregon containing 130‐yr‐old timber increased annual water yield up to 42 cm. For 4 years after logging, yield increases averaged 38 cm at a 13.0‐ha clearcut watershed and 20 cm at a 15.4‐ha watershed where timber was shelterwood cut. Increased summer flows were indicated by much fewer low‐flow days after logging, particularly at the clearcut watershed. During the 1977 drought year, only eight and two low‐flow days occurred at the clearcut and shelterwood cut watersheds, respectively, compared to 143 and 135 low‐flow days predicted by the calibration relationship. Neither the size nor the timing of peak flows changed significantly after logging at either watershed.
Water Resources Research – Wiley
Published: Jun 1, 1982
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