Access the full text.
Sign up today, get DeepDyve free for 14 days.
D. Spittlehouse, T. Black (1980)
Evaluation of the Bowen ratio/energy balance method for determining forest evapotranspirationAtmosphere-ocean, 18
M. Sharma, R. Luxmoore (1979)
Soil spatial variability and its consequences on simulated water balanceWater Resources Research, 15
K. Mcnaughton, T. Black (1973)
A study of evapotranspiration from a Douglas fir forest using the energy balance approachWater Resources Research, 9
S. Idso (1980)
On the apparent incompatibility of different atmospheric thermal radiation data setsQuarterly Journal of the Royal Meteorological Society, 106
J. Gash (1978)
Comment on the paper by A. S. Thom and H. R. Oliver ‘On penman's equation for estimating regional evaporation’ (Q.J., 1977, 103, 345–357)Quarterly Journal of the Royal Meteorological Society, 104
H. Item (1978)
A model for the water regime of coniferous forest and grasslandJournal of Hydrology, 37
C. Thornthwaite, J. Mather (1955)
Instructions and tables for computing potential evapotranspiration and the water balance
C. Federer, D. Lash (1978)
Simulated streamflow response to possible differences in transpiration among species of hardwood treesWater Resources Research, 14
T. Black, W. Gardner, G. Thurtell (1969)
The Prediction of Evaporation, Drainage, and Soil Water Storage for a Bare SoilSoil Science Society of America Journal, 33
W. Shuttleworth, I. Calder (1979)
Has the Priestley-Taylor Equation Any Relevance to Forest Evaporation?Journal of Applied Meteorology, 18
Gash Gash (1978)
Comments on the paper by A. S. Thom and H. R. Oliver, ‘On Penman's equation for estimating regional evaporation,’Quart. J. R. Meteorol. Soc., 104
C. Federer (1979)
A soil-plant-atmosphere model for transpiration and availability of soil waterWater Resources Research, 15
R. Harr (1977)
Water flux in soil and subsoil on a steep forested slopeJournal of Hydrology, 33
D. Hillel, C. Bavel (1976)
Simulation of Profile Water Storage as Related to Soil Hydraulic Properties1Soil Science Society of America Journal, 40
R. Jackson, S. Idso, R. Reginato (1976)
Calculation of evaporation rates during the transition from energy-limiting to soil-limiting phases using albedo dataWater Resources Research, 12
T. Black (1979)
Evapotranspiration from Douglas fir stands exposed to soil water deficitsWater Resources Research, 15
Black Black, Gardner Gardner, Thurtell Thurtell (1969)
The prediction of evaporation, drainage and water storage for a bare soilSoil Sci. Soc. Am. Proc., 33
J. Aase, S. Idso (1978)
A comparison of two formula types for calculating long‐wave radiation from the atmosphereWater Resources Research, 14
W. Emmingham, R. Waring (1977)
An index of photosynthesis for comparing forest sites in western OregonCanadian Journal of Forest Research, 7
K. King (1961)
Evaporation from land surfaces, 2
D. Spittlehouse (1981)
Measuring and modelling evapotranspiration from Douglas-fir stands
A. Plamondon (1972)
Hydrologic properties and water balance of the forest floor of a Canadian west coast watershed
J. Stewart (1977)
Evaporation from the wet canopy of a pine forestWater Resources Research, 13
K. Mcnaughton (1976)
Evaporation and advection I: evaporation from extensive homogeneous surfacesQuarterly Journal of the Royal Meteorological Society, 102
Wijk Wijk, Vries Vries (1954)
EvapotranspirationNeth. J. Agric. Sci., 2
C. Tan, T. Black, J. Nnyamah (1978)
A Simple Diffusion Model of Transpiration Applied to a Thinned Douglas‐Fir StandEcology, 59
I. Cowan (1965)
Transport of Water in the Soil-Plant-Atmosphere SystemJournal of Applied Ecology, 2
J. Nnyamah, T. Black (1977)
Rates and Patterns of Water Uptake in a Douglas-Fir Forest1Soil Science Society of America Journal, 41
H. Bruin, J. Keijman (1979)
The Priestley-Taylor Evaporation Model Applied to a Large, Shallow Lake in the NetherlandsJournal of Applied Meteorology, 18
B. Clothier, D. Scotter, J. Kerr (1977)
Drainage Flux in Permeable Soil Underlain by a Coarse-Textured Layer 1Soil Science Society of America Journal, 41
Refinement in empirical functions for realistic soil - moisture regimes under forest cover
G. Campbell (1974)
A SIMPLE METHOD FOR DETERMINING UNSATURATED CONDUCTIVITY FROM MOISTURE RETENTION DATASoil Science, 117
D. Spittlehouse, T. Black (1981)
Measuring and modelling forest evapotranspirationCanadian Journal of Chemical Engineering, 59
C. Priestley, R. Taylor (1972)
On the Assessment of Surface Heat Flux and Evaporation Using Large-Scale ParametersMonthly Weather Review, 100
W. Jury, C. Tanner (1975)
Advection Modification of the Priestley and Taylor Evapotranspiration Formula1Agronomy Journal, 67
R. Clapp, G. Hornberger (1978)
Empirical equations for some soil hydraulic propertiesWater Resources Research, 14
The forest water balance model presented requires only daily solar radiation, maximum and minimum air temperature, and rainfall as the input weather data. Site parameters are root zone depth, soil water retention and drainage characteristics, estimated canopy leaf area index, and the coefficients of the evapotranspiration and rainfall interception submodels. The evapotranspiration submodel calculates the forest evapotranspiration rate as the lesser of energy‐limited and soil‐limited rates. The former is calculated from the 24‐hour net radiation and the latter from the fraction of extractable water in the root zone. Solar radiation and air temperature are used to calculate net radiation. Interception is calculated from the daily rainfall. The root zone is treated as a single layer with drainage calculated as a function of the root zone water content. Water deficits and the matric potential of the root zone are used to indicate tree Water stress. The model was tested on two Douglas fir stands of different stand density and leaf area index. The coefficients used in the evapotranspiration submodel were found to be the same for both stands. It was also found that over 20% of the growing season rainfall was lost through interception.
Water Resources Research – Wiley
Published: Dec 1, 1981
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.