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| The '''Bradshaw Model''' is a geographical model which describes how a river's characteristics vary between the ] and ] of a ]. It shows that discharge, occupied channel width, channel depth and average load quantity increases downstream. Load particle size, channel bed roughness and gradient are all characteristics which decrease ]. |
The '''Bradshaw Model''' is a geographical model which describes how a river's characteristics vary between the ] and ] of a ]. It shows that discharge, occupied channel width, channel depth and average load quantity increases downstream. Load particle size, channel bed roughness and gradient are all characteristics which decrease ]. | ||
| ==External links== | ==External links== | ||
Revision as of 08:52, 30 April 2007
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The Bradshaw Model is a geographical model which describes how a river's characteristics vary between the lower course and upper course of a river. It shows that discharge, occupied channel width, channel depth and average load quantity increases downstream. Load particle size, channel bed roughness and gradient are all characteristics which decrease downstream.
External links
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