Fr. Meng et al., THE NASHWAAK-EXPERIMENTAL-WATERSHED-PROJECT - ANALYZING EFFECTS OF CLEARCUTTING ON SOIL-TEMPERATURE, SOIL-MOISTURE, SNOWPACK, SNOWMELT AND STREAM-FLOW, Water, air and soil pollution, 82(1-2), 1995, pp. 363-374
A forest disturbance such as clearcutting affects local climate condit
ions by affecting surface reflectance, amount of snow catch, amount an
d timing of snowmelt and stream water discharge, soil moisture, soil t
emperature and soil frost. In this paper, snowpack water equivalents,
soil moisture and soil temperature are simulated for pre- and post-har
vest conditions at the Nashwaak Experimental Watershed Project. This P
roject involved a paired watershed experiment, with one of the forest-
covered basins cut by way of a conventional harvesting operation, and
the other basin left as a control. The computer simulations involved t
he application of a forest hydrology model (ForHyM) and a soil tempera
ture model (ForSTeM). Both models used monthly amounts of rain and sno
w and mean monthly air temperatures records as input. Forest-atmospher
e energy balances were calculated for year-round conditions. In this r
eport, special attention was given to the energy balance when the grou
nd is covered with snow. Doing so generated a process-oriented approac
h for calculating snowmelt throughout the winter and at the beginning
of spring. Year-round model simulations for stream discharge were comp
ared with pre- and post-harvest discharge observations. Also compared
were simulated and observed snowpack water equivalents. Simulated resu
lts were in good agreement with field observations, thereby supporting
the general calculations made for pre-and post-harvest soil moisture,
temperature and frost conditions. Altogether; it was found that clear
cutting produced positive as well as negative contributions to the wat
er budget of the harvested basin. Positive contributions were likely d
ue to reduced evapotranspiration. Negative contributions were likely d
ue to reduced snow and fog water catch. Increased ground-level insolat
ion advanced the snowmelt season for the cut basin by about two weeks.