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The '''Bradshaw Model''' is a geographical model which describes how a river's characteristics vary between the ] and ] of a ] 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 characterisitcs decrease ].

The '''Bradshaw model''' shows that discharge, occupied channel width, channel depth and average load quanity increases downstream. Load particle size, channel bed roughness and gradient are characterisitcs which decrease ].


==External links== ==External links==
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Revision as of 22:25, 22 February 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 characterisitcs decrease downstream.

External links


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