Early Effects of Forest Fire on Streamflow CharacteristicsPacific Northwest Forest and Range Experiment Station, Forest Service, U.S. Department of Agriculture, 1971 - Forest fires - 9 pages |
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H. W. Berndt. Higher flows after the fire may also be an effect of soil heat flux . Moisture migrates from surface layers to lower zones in response to transient thermal gradients produced by the daily temperature cycle . A massive heat ...
H. W. Berndt. Higher flows after the fire may also be an effect of soil heat flux . Moisture migrates from surface layers to lower zones in response to transient thermal gradients produced by the daily temperature cycle . A massive heat ...
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20 to September air temperature Alaska annual precipitation APRIL MAY JUNE AUG SEPT August 24 Burns and Fox BURNS CREEK Cascade Ceanothus change in flow daily DEGREES F diurnal fluctuations Douglas-fir drainage early morning east slope effects elevation Entiat Experimental Forest Entiat River basin FEB MAR APRIL Feet per Second Figure flow rates occur forest fire Fox Creeks glacier granodiorite headwater heat flux Hydrographs hydrologic Ignition INCHES installations instruments JUNE JULY late summer maximum insolation McCree Creek mean temperature moisture MONTHLY MEAN normal depletion curves OCT NOV DEC Oregon oscillating peak percent ponderosa pine preburn data precipitation occur precipitation was recorded pumice range reduction result rock Runoff snowmelt period soil species spring snowmelt storm stream gaging stream temperature Streamflow characteristics STREAMFLOW Cubic Feet streamside study area summer season TEMPERATURE DEGREES thermal gradients three streams transpiration draft tributary streams valley vegetative succession volcanic Washington WATER TEMPERATURE watersheds weir winter zones