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G. Tucker, Rudy Slingerland (1996)
Predicting sediment flux from fold and thrust beltsBasin Research, 8
(1990)
Interaction of weathering and transport processes in the evolution of arid landscapes Quantitative dynamic stratigraphy: Englewood Cliffs
D. Coates, J. Vitek (2020)
Thresholds in Geomorphology
G. Moglen (1995)
Simulation of observed topography using a physically-based basin evolution model
M. Melton (1958)
Correlation Structure of Morphometric Properties of Drainage Systems and Their Controlling AgentsThe Journal of Geology, 66
O'Loughlin O'Loughlin (1986)
Prediction of surface saturation zones in natural catchmentsWater Resour. Res., 22
(1996)
Modeling the large-scale interaction of climate, tectonics, and topography
M. Kirkby (2020)
A two-dimensional simulation model for slope and stream evolution
G. Tucker, Rudy Slingerland (1994)
Erosional dynamics, flexural isostasy, and long-lived escarpments: A numerical modeling studyJournal of Geophysical Research, 99
A. Howard (1994)
A detachment-limited model of drainage basin evolutionWater Resources Research, 30
S. Schumm (1963)
The disparity between present rates of denudation and orogeny
Willgoose Willgoose, Bras Bras, Rodríguez‐Iturbe Rodríguez‐Iturbe (1990)
A model of river basin evolutionEos Trans. AGU, 71
S. Schumm, R. Hadley (1961)
Progress in the application of landform analysis in studies of semiarid erosion
Rosenbloom Rosenbloom, Anderson Anderson (1994)
Hillslope and channel evolution in a marine terraced landscape, Santa Cruz, CaliforniaJ. Geophys. Res., 99
A. Howard (1997)
BADLAND MORPHOLOGY AND EVOLUTION: INTERPRETATION USING A SIMULATION MODELEarth Surface Processes and Landforms, 22
F. Ahnert (1970)
Functional relationships between denudation, relief, and uplift in large, mid-latitude drainage basinsAmerican Journal of Science, 268
G. Willgoose, R. Bras, I. Rodríguez‐Iturbe (1991)
A coupled channel network growth and hillslope evolution model: 1. TheoryWater Resources Research, 27
M. Kirkby, K. Beven (1979)
A physically based, variable contributing area model of basin hydrology, 24
G. Willgoose (1994)
A statistic for testing the elevation characteristics of landscape simulation modelsJournal of Geophysical Research, 99
(1992)
River mechanics
G. Willgoose, R. Bras, I. Rodríguez‐Iturbe (1990)
A model of river basin evolutionEos, Transactions American Geophysical Union, 71
(1993)
Long term interactions between networks and hillslopes
J. Knox (1983)
Responses of river systems to Holocene climates
A. Parsons, A. Abrahams, J. Wainwright (1994)
On determining resistance to interrill overland flowWater Resources Research, 30
Willgoose Willgoose, Bras Bras, Rodríguez‐Iturbe Rodríguez‐Iturbe (1991)
A physically based coupled network growth and hillslope evolution model, 1, TheoryWater Resour. Res., 27
W. Dietrich, C. Wilson, D. Montgomery, J. McKean (1993)
Analysis of Erosion Thresholds, Channel Networks, and Landscape Morphology Using a Digital Terrain ModelThe Journal of Geology, 101
D. Montgomery, W. Dietrich (1989)
Source areas, drainage density, and channel initiationWater Resources Research, 25
(1996)
Thresholds and bistable states in landform evolution models ( abstract )
E. Ijjász-Vásquez, R. Bras (1995)
Scaling regimes of local slope versus contributing area in digital elevation modelsGeomorphology, 12
R. Rigon, A. Rinaldo, I. Rodríguez‐Iturbe (1994)
On landscape self-organizationJournal of Geophysical Research, 99
J. Hack (1957)
Studies of longitudinal stream profiles in Virginia and Maryland
L. Leopold, T. Maddock (1953)
The hydraulic geometry of stream channels and some physiographic implications
Melton Melton (1958)
Correlation structure of morphometric pressure of drainage basins and their controlling agentsJ. Geol., 66
W. Dietrich, C. Wilson, D. Montgomery, J. McKean, R. Bauer (1992)
Erosion thresholds and land surface morphologyGeology, 20
(1978)
Field studies of hillslope flow processes
N. Lifton, C. Chase (1992)
Tectonic, climatic and lithologic influences on landscape fractal dimension and hypsometry : implications for landscape evolution in the San Gabriel Mountains, CaliforniaGeomorphology, 5
Modelling some influences of soil erosion , landslides and valley gradient on drainage density and hollow development
D. Nash (1980)
Morphologic Dating of Degraded Normal Fault ScarpsThe Journal of Geology, 88
D. Montgomery, E. Foufoula‐Georgiou (1993)
Channel network source representation using digital elevation modelsWater Resources Research, 29
Terence Smith, F. Bretherton (1972)
Stability and the conservation of mass in drainage basin evolutionWater Resources Research, 8
D. Tarboton, R. Bras, I. Rodríguez‐Iturbe (1991)
On the extraction of channel networks from digital elevation dataHydrological Processes, 5
(1987)
Process-response models of denudation at different spatial scales: Catena Supplement
N. Clifford (1996)
Classics in physical geography revisitedProgress in Physical Geography, 20
K. Gregory, V. Gardiner (1975)
Drainage density and climateZeitschrift für Geomorphologie
Y. Enzel, R. Amit, N. Porat, E. Zilberman, Bruce Harrison (1996)
Estimating the ages of fault scarps in the Arava, IsraelTectonophysics, 253
R. David, E. William (1994)
Landscape dissection and drainage area-slope thresholds, 221246
C. Beaumont, P. Fullsack, J. Hamilton (1992)
Erosional control of active compressional orogens
G. Moglen, E. Eltahir, R. Bras (1998)
On the sensitivity of drainage density to climate changeWater Resources Research, 34
T. Hanks, R. Bucknam, K. Lajoie, R. Wallace (1984)
Modification of wave-cut and faulting-controlled landformsJournal of Geophysical Research, 89
(1994)
Thresholds and instability in stream head hollows: a model of magnitude and frequency for wash processes
G. Tucker, Rudy Slingerland (1997)
Drainage basin responses to climate changeWater Resources Research, 33
S. Schumm (1956)
EVOLUTION OF DRAINAGE SYSTEMS AND SLOPES IN BADLANDS AT PERTH AMBOY, NEW JERSEYGeological Society of America Bulletin, 67
(1997)
The role of rainfall variability in drainage basin evolution: implications of a stochastic model
T. Oguchi (1997)
Drainage Density and Relative Relief in Humid Steep Mountains with Frequent Slope FailureEarth Surface Processes and Landforms, 22
I. Moore, G. Burch (1986)
Sediment Transport Capacity of Sheet and Rill Flow: Application of Unit Stream Power TheoryWater Resources Research, 22
Gregory Gregory, Gardiner Gardiner (1975)
Drainage density and climateZ. Geomorphol., Neue Folge, 19
G. Gilbert (1909)
The Convexity of HilltopsThe Journal of Geology, 17
S. Schumm, M. Mosley, W. Weaver (1987)
Experimental fluvial geomorphology
D. Montgomery, W. Dietrich (1994)
A physically based model for the topographic control on shallow landslidingWater Resources Research, 30
Downstream fining : A drainage basin perspective ( abstract )
A. Rinaldo, W. Dietrich, R. Rigon, Gregory Vogel, Ignacio Rodrlguez-lturbe (1995)
Geomorphological signatures of varying climateNature, 374
Ahnert (1987)
Process-response models of denudation at different spatial scalesCatena Suppl., 10
(1987)
Modelling fluvial systems: rock-, gravel-and sand-bed channels River channels
D. Loewenherz (1991)
Stability and the initiation of channelized surface drainage: A reassessment of the short wavelength limitJournal of Geophysical Research, 96
M. Summerfield, N. Hulton (1994)
Natural controls of fluvial denudation rates in major world drainage basinsJournal of Geophysical Research, 99
D. Montgomery, W. Dietrich (1992)
Channel Initiation and the Problem of Landscape ScaleScience, 255
E. Ijjász-Vásquez, R. Bras, G. Moglen (1992)
Sensitivity of a basin evolution model to the nature of runoff production and to initial conditionsWater Resources Research, 28
R. Horton (1945)
EROSIONAL DEVELOPMENT OF STREAMS AND THEIR DRAINAGE BASINS; HYDROPHYSICAL APPROACH TO QUANTITATIVE MORPHOLOGYGeological Society of America Bulletin, 56
P. Eagleson (1978)
Climate, soil, and vegetation: 2. The distribution of annual precipitation derived from observed storm sequencesWater Resources Research, 14
M. Melton (1958)
Geometric Properties of Mature Drainage Systems and Their Representation in an E4 Phase SpaceThe Journal of Geology, 66
E. O'Loughlin (1986)
Prediction of Surface Saturation Zones in Natural Catchments by Topographic AnalysisWater Resources Research, 22
D. Tarboton, R. Bras, I. Rodríguez‐Iturbe (1992)
A Physical Basis for Drainage DensityGeomorphology, 5
N. Rosenbloom, R. Anderson (1994)
Hillslope and channel evolution in a marine terraced landscape
Catchment morphology and drainage density are strongly influenced by hillslope processes. The consequences of several different hillslope process laws are explored in a series of experiments with a numerical model of drainage basin evolution. Five different models are considered, including a simple diffusive‐advective process transition, a runoff generation threshold, an erosion threshold, and two types of threshold‐activated landsliding. These different hillslope processes alter both the visual appearance of the landscape and the predicted relationship between slope and contributing area. On the basis of the different threshold theories, we derive expressions for the relationships between drainage density and environmental factors such as rainfall, relief, and mean erosion rate. These relationships vary depending on the dominant hillslope threshold. In particular, the sign of the predicted relationship between drainage density and relief is positive in semiarid, low‐relief landscapes and negative in humid landscapes dominated by a saturation threshold and/or in high‐relief landscapes dominated by simple threshold landsliding.
Water Resources Research – Wiley
Published: Oct 1, 1998
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