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The Bradshaw model (Discharge (increases downstream (because tributaries…
The Bradshaw model
Discharge
increases downstream
because tributaries add to the total amount of water
measured in Cumecs (m3/s)
Channel width
increase downstream
because tributaries add to the total amount of water
measured in cm
Channel depth
increases downstream
because tributaries add to the total amount of water
measured in cm
Average velocity
increases downstream
measured in m/s
Load quantity
increases downstream
Load particle size
decreases downstream
because attrition breaks down the edges of the particles
Channel bed roughness
decreases downstream
because attrition breaks down the edges of the particles
Slope angle gradient
Decreases downstream