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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 quanity increases downstream. Load particle size, channel bed roughness and gradient are |
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 quanity increases downstream. Load particle size, channel bed roughness and gradient are all characteristics which decrease ]. | ||
| ==External links== | ==External links== | ||
Revision as of 00:32, 17 March 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 quanity increases downstream. Load particle size, channel bed roughness and gradient are all characteristics which decrease downstream.
External links
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