The dominant channel forming discharge is often assumed to be the bankfull flow.
For example Knighton (1998) argued that "since it seems reasonable to suppose that river channels are adjusted on average to a flow which just fills the available cross-section, dominant discharge has been equated with bankfull flow, thereby giving it additional
morphogenetic significance."
The dominant discharge is supposed to give the same effects as the whole range of
discharges occurring (Brandt, 2000).
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Brandt, S.A., 2000: Classification of geomorphological effects downstream of dams. Catena, vol. 40(4), pp. 375-401. doi:10.1016/S0341-8162(00)00093-X Knighton, D., 1998. Fluvial Forms and Processes: A New Perspective. Arnold, London, xv+383 pp.
Bankfull width refers to the width of a river or stream when it is at maximum capacity, just before it begins to overflow its banks. It is a key measurement used in river management and flood forecasting to help determine potential flood levels.
Hydrology is like oceanography in that both involve the study of currents and their effect overall on the bodies of ocean water. Hydrology is different because unlike oceanography, it deals solely with the movement of the water.
Hydrology is a branch of physical geography and hydrology is the study of weather and weather natural (physical not human) P.S: don't get confused its physical not human because people only study weather
For horseisle, the answer is water /////Dreygon on roan\\\\\
Surface water hydrology and groundwater hydrology both affect the terrain. Surface water hydrology refers to the movement and distribution of water on the Earth's surface through processes like erosion and sediment transport, which can shape the terrain over time. Groundwater hydrology involves the movement of water beneath the Earth's surface, which can lead to processes like karst formation or the creation of underground aquifers that influence the terrain above.
It depends how far along the river course it is. In theory as you move further down the river's course the bankfull width should increase.
Bankfull width refers to the width of a river or stream when it is at maximum capacity, just before it begins to overflow its banks. It is a key measurement used in river management and flood forecasting to help determine potential flood levels.
The brakes in my car are hydraulic.
I am searching for an introductory class in hydrology.
Alexandra P. Wright has written: 'Environmental geology and hydrology, Tampa area, Florida' -- subject(s): Geology, Hydrology, Land use
River width refers to the distance across a river from one bank to the opposite bank. It can vary significantly along a river's course due to factors such as topography, sediment deposition, and flow dynamics. Measuring the width of a river is important for understanding its hydrology, ecology, and potential for flooding. Additionally, river width can influence navigation, habitat availability, and water quality.
H. E. Mahood has written: '1974 spring runoff in the Souris River Basin, Saskatchewan' -- subject(s): Runoff 'Upper Carrot River hydrology study' -- subject(s): Hydrology 'Frenchman River basin hydrology study' -- subject(s): Hydrology, Water-supply 'Chaplin Lake Basin hydrology study' -- subject(s): Hydrology 'Wood River near Gravelbourg hydrology study' -- subject(s): Hydrology
Numismatics
Hydrology - album - was created on 1988-01-25.
the tool used to find the width of a pencil is a ruler. But use the centimeter side of it for the width only!!
No. Hydrology deals with reseviours and subsurface waters also.
John E. Gribbin has written: 'Introduction to Hydraulics & Hydrology' 'Hydraulics and hydrology for stormwater management' -- subject(s): Hydraulics, Management, Hydrology, Urban runoff