Premium
Measured differences in snow accumulation and melt among clearcut, juvenile, and mature forests in southern British Columbia
Author(s) -
Winkler R. D.,
Spittlehouse D. L.,
Golding D. L.
Publication year - 2005
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.5757
Subject(s) - abies lasiocarpa , picea engelmannii , pinus contorta , snowmelt , snow , juvenile , environmental science , snowpack , subalpine forest , forestry , ecology , hydrology (agriculture) , physical geography , atmospheric sciences , biology , geography , montane ecology , geology , meteorology , geotechnical engineering
Quantification of the relationships between snow and forest cover, including its removal through logging, insects or disease and its regrowth, is a prerequisite to assessing the effects of forestry practices on streamflow from montane and boreal forest watersheds. Over a 3 year period, a juvenile and a juvenile‐thinned lodgepole pine ( Pinus contorta Dougl.) stand, a mature mixed Engelmann spruce ( Picea engelmannii Parry), subalpine fir ( Abies lasiocarpa (Hook.) Nutt) and lodgepole pine stand, and a clearcut were intensively surveyed to quantify differences in snow water equivalent (SWE). Daily snowmelt, weather conditions, and the energy balance were measured during the first year of this study. The 1 April SWE was 32% and 14% less under the mature and juvenile forests respectively than in the clearcut. No significant differences in peak SWE were measured between the juvenile and juvenile‐thinned stands. Continuous snowmelt lysimeter measurements showed that snowmelt began earlier, accumulated more rapidly, and disappeared 2 to 4 days earlier in the juvenile‐thinned stand than in either the unthinned juvenile stand or the clearcut. When the snowpack had disappeared from the clearcut and juvenile stands, 30% of the SWE on 1 April remained in the mature forest. The results not only show that snow accumulation and melt differ significantly between clearcut, juvenile, and mature stands, but also that snowmelt patterns vary among juvenile stands with distinct structural differences. This is due to the difference in the energy balances, dominated by radiant heat fluxes, of the four sites. Copyright © 2005 John Wiley & Sons, Ltd.