Geoscience Reference
In-Depth Information
outperform lumped models. In other words, there isstill no general consensus regarding
the optimal simplifying assumptions that are most appropriate to describe streamflow
generation under a given set of conditions. Although it could be argued that there never
will be a consensus, this field is inanactive state of development and rapid advances
continue to be made.
REFERENCES
Abdul, A. S. and Gillham, R. W. (1989). Field studies of the effects of the capillary fringe on
streamflow. J. Hydrol. , 112 , 1-18.
Beven, K. and Germann, P. (1982). Macropores and water flow insoils. Water Resour. Res. , 18 ,
1311-1325.
Bonnell, M. and Gilmour, D. A. (1978). The development of overland flow in a tropical rainforest
catchment. J. Hydrol. , 39 , 365-382.
Brown, V. A., McDonnell, J. J., Burns, D. A. and Kendall, C. (1999). The role of event water, a rapid
shallow flow component, and catchment size in summer stormflow. J. Hydrol. , 217 , 171-190.
Chappell, N. A., Ternan, J. L.,Williams, A. G. and Reynolds, B. (1990). Preliminary analysis of water
and solute movement beneath a coniferous hillslope inmid-Wales, U.K. J. Hydrol. , 116 ,
201-215.
Dooge, J. C. I. (1957). The rational method for estimating flood peaks. Engineering (London) , 184 ,
311-313, 374-377.
(1973). Linear theory of hydrologic systems , Tech. Bull. 1468. Washington, DC: Agric. Res. Serv.,
US Department of Agriculture.
Dunne, T. and Black, R. D. (1970a). An experimental investigation of runoff production in permeable
soils. Water Resour. Res. , 6 , 478-490.
(1970b). Partial area contributions to storm runoff in a small New England watershed. Water Resour.
Res. , 6 , 1296-1311.
Elsenbeer, H. (2001). Hydrologic flowpaths in tropical rainforest soilscapes-areview. Hydrological
Processes , 15 , 1751-1759.
Elsenbeer, H., Lorieri,D. and Bonnell, M. (1995a). Mixing model approaches to estimate stormflow
sources in an overland flow-dominated tropical rainforest catchment. Water Resour. Res. , 31 ,
2267-2278.
Elsenbeer, H., Lack, A. and Cassel, K. (1995b). Chemical fingerprints of hydrological compartments
and flow paths at La Cuenca, western Amazonia. Water Resour. Res. , 31 , 3051-3058.
Glass, R. J., Steenhuis, T. S. and Parlange, J.-Y. (1989). Mechanism for finger persistence in
homogeneous, unsaturated, porous media: theory and verification. Soil Sci. , 148 , 60-70.
Hawker, W. H. and Ross, C. N. (1921). The calculation of flood discharges by the use of a time contour
plan. Trans. Inst. Engrs Aust. , 2 , 85-92.
Hewlett, J. D. (1974). Comments on letters relating to 'Role of subsurface flow in generating surface
runoff, 2, Upstream source areas' by R. Allan Freeze. Water Resour. Res. , 10 , 605-607.
Hewlett, J. D. and Hibbert, A. R. (1963). Moisture and energy conditions within a sloping soil mass
during drainage. J. Geophys. Res. , 68 , 1081-1087.
(1967). Factors affecting the response of small watersheds to precipitation in humid areas. In Forest
Hydrology ,ed. W. E. Sopper and H. W. Lull. New York: Pergamon Press, pp. 275-290.
Horton, R. E. (1932). Drainage-basin characteristics. Trans. Amer. Geophys. Un. , 13 , 350-361.
(1933). The role of infiltration in the hydrologic cycle. Trans. Amer. Geophys. Un. , 14 , 446-460.
Search WWH ::




Custom Search