Channel network hydrology
Using an interdisciplinary approach, it combines the results of recent research on the form and function of channel networks and their role in controlling hydrological responses. Addresses both the processes involved in short term responses and the longer term behavior of these networks. The understanding gained from experiments and fieldwork is reflected in an up-to-date summary.
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BATHURST Water Resource Systems Research Unit Department of Civil
Extraction of Channel Networks and Topographic Parameters from Digital
The Geomorphological Unit Hydrograph
8 other sections not shown
advection ADZ model analysis approach approximation average bed material bedform bedload Beven boundary catchment chan channel head channel network characteristics climate coefficient colluvium concentration constant convex cross-sectional dead zone delivery ratio depth Dietrich diffusion discharge dispersion distance distribution downcutting downslope downstream drainage area drainage basin drainage density effect elevation Engrs equation estimated Fischer flow resistance form drag function geomorphological gradient headcut hillslope Horton overland flow hydraulic hydrograph hydrological hydrological response incision increase input kinematic wave Kirkby length longitudinal ment method overland flow parameters peak pixel predicted Proc processes rainfall regolith relationship River River Hodder Rodriguez-Iturbe roughness routing runoff saturated scale sedi sediment delivery sediment transport sediment yield shear stress slope profiles soil solute source-basin spatial storage storm stream subsurface flow surface threshold tion topographic turbulent upslope upstream valley values variables variation Water Resources Research watershed width