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Rodger D.Moore (1992)
Effect Of Land-Surface Configuration On Catchment Hydrology
M. Kirkby, R. Chorley (1967)
THROUGHFLOW, OVERLAND FLOW AND EROSIONHydrological Sciences Journal-journal Des Sciences Hydrologiques, 12
Brakensiek Brakensiek (1967)
Kinematic flood routingTrans. Am. Soc. Agric. Eng., 10
D. Zasłavsky, G. Sinai (1981)
Surface Hydrology: I—Explanation of PhenomenaJournal of Hydraulic Engineering, 107
R. Grayson, I. Moore, T. McMahon (1992)
Physically based hydrologic modeling: 1. A terrain‐based model for investigative purposesWater Resources Research, 28
D. Zasłavsky, A. Rogowski (1969)
Hydrologic and Morphologic Implications of Anisotropy and Infiltration in Soil Profile Development1Soil Science Society of America Journal, 33
P. Troch, M. Mancini, C. Paniconi, E. Wood (1993)
Evaluation of a distributed catchment scale water balance modelWater Resources Research, 29
K. Beven (1981)
Kinematic subsurface stormflowWater Resources Research, 17
I. Moore, R. Grayson (1991)
Terrain‐based catchment partitioning and runoff prediction using vector elevation dataWater Resources Research, 27
Zaslavsky Zaslavsky, Sinai Sinai (1981)
Surface hydrology, I, Explanation of phenomenaJ. Hydraul. Div. Am. Soc. Civ. Eng., 107
M. Anderson, P. Kneale (1982)
The influence of low-angled topography on hillslope soil-water convergence and stream dischargeJournal of Hydrology, 57
I. Moore, G. Burch, D. Mackenzie (1988)
Topographic Effects on the Distribution of Surface Soil Water and the Location of Ephemeral GulliesTransactions of the ASABE, 31
Anderson (1978)
Experimental investigations concerning the topographic control of soil water movement on hillslopesZ. Geomorph., 29
Zaslavsky Zaslavsky, Rogowski Rogowski (1969)
Hydrologic and morphologic implications of anisotropy and infiltration in soil profile developmentSoil Sci. Soc. Am. Proc., 33
M. Sivapalan, K. Beven, E. Wood (1987)
On hydrologic similarity: 2. A scaled model of storm runoff productionWater Resources Research, 23
K. Beven, M. Kirkby, N. Schofield, A. Tagg (1984)
Testing a physically-based flood forecasting model (TOPMODEL) for three U.K. catchmentsJournal of Hydrology, 69
E. O'Loughlin, D. Short, W. Dawes (1989)
Modelling the Hydrological Response of Catchments to Land Use Change
I. Moore, T. Norton, Jann Williams (1993)
Modelling environmental heterogeneity in forested landscapesJournal of Hydrology, 150
D. Yaalon, D. Kalmar (1978)
Dynamics of cracking and swelling clay soils: Displacement of skeletal grains, optimum depth of slickensides, and rate of intra‐pedonic turbationEarth Surface Processes and Landforms, 3
Iida Iida (1984)
A hydrological method of estimation of topographic effect on saturated throughflowTrans. Jap. Geomorphol. Union, 5
Zaslavsky Zaslavsky, Sinai Sinai (1981)
Surface hydrology, III, Causes of lateral flowJ. Hydraul. Div. Am. Soc. Civ. Eng., 107
Moore Moore, Burch Burch, Mackenzie Mackenzie (1988)
Topographic effects on the distribution of surface soil water and the location of ephemeral gulliesTrans. Am. Soc. Agric. Eng., 31
J. McCord, D. Stephens (1987)
Lateral moisture flow beneath a sandy hillslope without an apparent impeding layerHydrological Processes, 1
M. Kirkby, K. Beven (1979)
A physically based, variable contributing area model of basin hydrology, 24
A. Ladson, I. Moore (1992)
Soil water prediction on the Konza Prairie by microwave remote sensing and topographic attributesJournal of Hydrology, 138
M. Anderson, P. Kneale (1980)
Topography and hillslope soil water relationships in a catchment of low reliefJournal of Hydrology, 47
M. Anderson, T. Burt (1978)
The role of topography in controlling throughflow generationEarth Surface Processes and Landforms, 3
K. Beven (1982)
On subsurface stormflow: an analysis of response timesHydrological Sciences Journal-journal Des Sciences Hydrologiques, 27
P. Sloan, I. Moore (1984)
Modeling subsurface stormflow on steeply sloping forested watershedsWater Resources Research, 20
I. Moore, R. Grayson, A. Ladson (1991)
Digital terrain modelling: A review of hydrological, geomorphological, and biological applicationsHydrological Processes, 5
Kirkby Kirkby, Chorley Chorley (1967)
Throughflow, overland flow and erosionBull. Int. Assoc. Sci. Hydrol., 12
D. Brakensiek (1967)
Kinematic Flood RoutingTransactions of the ASABE, 10
I. Moore, E. O'Loughlin, G. Burch (1988)
A contour‐based topographic model for hydrological and ecological applicationsEarth Surface Processes and Landforms, 13
E. Wood, M. Sivapalan, K. Beven (1990)
Similarity and scale in catchment storm responseReviews of Geophysics, 28
R. Whipkey (1965)
SUBSURFACE STORMFLOW FROM FORESTED SLOPESHydrological Sciences Journal-journal Des Sciences Hydrologiques, 10
R. Grayson (1990)
Terrain-based hydrologic modelling for erosion studies
Jones Jones (1986)
Some limitations to the a/s index for predicting basin‐wide patterns of soil water drainageZ. Geomorph., 60
R. Horton (1945)
EROSIONAL DEVELOPMENT OF STREAMS AND THEIR DRAINAGE BASINS; HYDROPHYSICAL APPROACH TO QUANTITATIVE MORPHOLOGYGeological Society of America Bulletin, 56
Whipkey Whipkey (1965)
Subsurface stormflow from forested slopesInt. Assoc. Sci. Hydrol. Bull., 10
J. Jones (1987)
The initiation of natural drainage networksProgress in Physical Geography, 11
E. O'Loughlin (1986)
Prediction of Surface Saturation Zones in Natural Catchments by Topographic AnalysisWater Resources Research, 22
J. Jones (1987)
The effects of soil piping on contributing areas and erosion patternsEarth Surface Processes and Landforms, 12
K. Beven, E. Wood (1983)
Catchment geomorphology and the dynamics of runoff contributing areasJournal of Hydrology, 65
D. Zasłavsky, G. Sinai (1981)
Surface Hydrology: III°Causes of Lateral FlowJournal of Hydraulic Engineering, 107
A quasi‐dynamic wetness index that accounts for variable drainage times since a prior rainfall event is derived from simple subsurface flow theory. The method is tested through a series of field observations and numerical experiments using a spatially distributed, dynamic hydrologic model. The quasi‐dynamic wetness index is shown to be a useful extension of previously developed static indices for predicting the location of zones of soil saturation and the distribution of soil water (i.e., the soil water content overlying a shallow impermeable or semiimpermeable layer). The new index is not constrained by the steady state assumption that forms the basis of existing indices.
Water Resources Research – Wiley
Published: Apr 1, 1994
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