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Modeling increases in snowmelt yield and desynchronization resulting from forest gap-thinning treatments in a northern mountain headwater basin
snowmelt yield desynchronization resulting mountain headwater basin
2014/4/3
A physically based model built upon extensive field observations of radiation dynamics
and snow processes in cold regions forest environments was used to investigate the impacts
of prescribed ...
Sensitivity of snowmelt hydrology in Marmot Creek, Alberta, to forest cover disturbance
forest snow Canadian Rocky Mountains pine beetle fi re clear-cutting
2014/4/3
A model including slope effects on snow redistribution, interception and energetics was developed using the Cold Regions
Hydrological Model platform, parameterized with minimal calibration and manipu...
Effects of needleleaf forest cover on radiation and snowmelt dynamics in the Canadian Rocky Mountains
radiation snowmelt dynamics Canadian Rocky Mountains
2014/4/3
Radiation is the main energy source for snowpack warming and melt in mountain needleleaf forests, and runoff
from these forests is the main contributor to spring river flows in western North America....
Simulation of snow accumulation and melt in needleleaf forest environments
needleleaf forest environments snow accumulation
2014/4/3
Drawing upon numerous field studies and modelling exercises of snow processes, the Cold Regions Hydrological Model (CRHM) was developed to simulate the four
season hydrological cycle in cold re...
A hillslope forest floor (duff) water budget and the transition to local control
forest fl oor water budget hillslope hydrology local control duff layer
2014/4/3
The partially decomposed organic layer (duff: F and H layers) of the forest floor is an important boundary between the soil
and atmospheric processes. Here we use both empirical data and a thre...
Runoff Generating Processes in Boreal Forest Environments with Glacial Tills
Runoff Generating Processes Boreal Forest Environments Glacial Tills
2009/10/22
This review describes the processes by which runoff is generated from rain or
snowmelt in a boreal forest landscape with a shallow layer of glacial tills overlying
a relatively impermeable bedrock. ...
Effect of Potential Warming on Evapotranspiration from Forest Catchments in Karelia
Effect of Potential Warming Evapotranspiration Forest Catchments
2009/10/22
The amount of evapotranspiration from a woodland largely depends on the site
and stand productivity. The factor largely responsible for the stand productivity
(productivity class) of an individual f...
RAINFALL PARTITIONING IN A MIXED WHITE OAK FOREST WITH DWARF BAMBOO UNDERGROWTH
RAINFALL PARTITIONING BAMBOO MIXED WHITE OAK FOREST
2009/10/19
Throughfall measurements in a 60-year-old white oak (Konara) stand (Quercus serrata THUNB.) with under growing dwarf bamboo (Sasa paniculata) were carried out during two periods totaling eleven months...
A conceptual model of daily water balance following partial clearing from forest to pasture
daily water balance streamflow generation processes
2009/5/13
A simple conceptual water balance model representing the streamflow generation processes on a daily time step following land use change is presented. The model consists of five stores: (i) Dry, Wet a...
Comparison of Rainfall-Runoff Characteristics in Forested Catchments Underlain by Granitic and Sedimentary Rock with Various Forest Age
rainfall-runoff Granitic Sedimentary Rock Various Forest Age
2009/4/13
This study examines rainfall-runoff characteristics of catchments underlain by granitic and sedimentary rock. Differences in bedrock geology and forest age for sedimentary rock catchments were conside...
Snowpack calibration on Mannot Creek to detect changes in accumulation pattern after forest-cover manipulation
Snowpack calibration forest-cover manipulation
2014/4/3
The calibration procedure commonly used in detecting
streamflow changes from a treated watershed was used for snow-accumulation changes resulting from watershed treatment . Nine...