Geoscience Reference
In-Depth Information
Brown, K. W. and Rosenberg, N. J. (1977). Resistance model to predict evapotranspiration and its
application to a sugarbeet field. Agronomy J. , 65 , 341-347.
Brubaker, K. L., Entekhabi,D. and Eagleson, P. S. (1994). Atmospheric water vapor transport and
continental hydrology over the Americas. J. Hydrology , 155 , 409-430.
Brutsaert, W. (1982). Evaporation into the Atmosphere: Theory, History and Applications . Dordrecht,
Holland/Boston, USA: D. Reidel Pub. Co.
Brutsaert, W. and Chan, F. K.-F. (1978). Similarity functions D for water vapor in the unstable
atmospheric boundary layer. Bound.-Layer Met. , 14 , 441-456.
Brutsaert, W. and Chen, D. (1996). Diurnal variation of surface fluxes during thorough drying (or
severe drought) of natural prairie. Water Resour. Res. , 32 , 2013-2019.
Brutsaert, W. and Stricker, H. (1979). An advection-aridity approach to estimate actual regional
evapotranspiration. Water Resour. Res. , 15 , 443-450.
Brutsaert, W. and Sugita, M. (1992). Application of self-preservation in the diurnal evolution
of the surface energy budget to determine daily evaporation. J. Geophys. Res. , 97 (D17),
18 377-18 382.
Brutsaert, W. and Yu, S.-L. (1968). Mass transfer aspects of pan evaporation. J. Appl. Met. , 7 ,
563-566.
Budyko, M. I. (1955). On the determination of evaporation from the land surface. Meteorol. Gidrol. , 1 ,
52-58 (in Russian).
(1974). Climate and Life . New York: Academic Press.
Carson, D. J. (1982). Current parametrizations of land-surface processes in atmospheric general
circulation models. In Land Surface Processes in Atmospheric General Circulation Models ,ed.
P. S. Eagleson. New York: Cambridge University Press, pp. 67-108.
Champagne, F. H.,Friehe, C. A., LaRue, J. C. and Wyngaard, J. C. (1977). Flux measurements, flux
estimation techniques and fine-scale turbulence measurements in the unstable surface layer over
land. J. Atmos. Sci. , 34 , 515-530.
Chen, D. and Brutsaert, W. (1995). Diagnostics of land surface spatial variability and water vapor flux.
J. Geophys. Res. , 100 (D12), 25, 595-525, 606.
Choudhury, B. J. and Blanchard, B. J. (1983). Simulating soil water recession coefficients for
agricultural watersheds. Water Resour. Bull. , 19 , 241-247.
Crago, R. D. (1996). A comparison of the evaporative fraction and the Priestley-Taylor parameter α for
parameterizing daytime evaporation. Water Resour. Res. , 32 , 1403-1409.
Crago, R. D. and Brutsaert, W. (1992). A comparison of several evaporation equations. Water Resour.
Res. , 28 , 951-954.
(1996). Daytime evaporation and the self-preservation of the evaporative fraction and the Bowen
ratio. J. Hydrol. , 178 , 241-255.
Daniel, J. F. (1976). Estimating groundwater evapotranspiration from streamflow records. Water
Resour. Res. , 12 , 360-364.
Davidson, J. M., Stone, L. R.,Nielsen, D. R. and La Rue, M. E. (1969). Field measurement and use of
soil-water properties. Water Resour. Res. , 5 , 1312-1321.
Davies, J. A. and Allen, C. D. (1973). Equilibrium, potential and actual evaporation from cropped
surfaces in southern Ontario. J. Appl. Met ., 12 , 649-657.
Dias, N. L. and Brutsaert, W. (1996). Similarity of scalars under stable conditions. Bound.-Layer Met. ,
80 , 355-373.
Dias, N. L. and Kan, A. (1999). A hydrometeorological model for basin-wide seasonal
evapotranspiration. Water Resour. Res. , 35 , 3409-3418.
Search WWH ::




Custom Search