Revision as of 17:01, 31 December 2014 editClueBot NG (talk | contribs)Bots, Pending changes reviewers, Rollbackers6,439,037 editsm Reverting possible vandalism by 90.41.124.129 to version by Widr. False positive? Report it. Thanks, ClueBot NG. (2076173) (Bot)← Previous edit | Revision as of 09:47, 22 May 2015 edit undo217.33.42.194 (talk) giiiiiiiiNext edit → | ||
Line 1: | Line 1: | ||
{{One source|date=September 2012}} | {{One source|date=September 2012}} | ||
The '''Bradshaw Model''' is a geographical model which describes how a river's characteristics vary between the ''upper course'' and ''lower course'' of a river. It shows that ], occupied channel width, channel depth and average load quantity increases downstream. Load |
The '''Bradshaw Model''' is a geographical model which describes how a river's characteristics vary between the ''upper course'' and ''lower course'' of a river. It shows that ], occupied channel width, channel depth and average load quantity increases downstream. Load le size, channel bed roughness and gradient are all characteristics that decrease; it is represented by triangles, of diffe rivers fit the model perfectly therefore the model is usually used in order to compare natural rivers to concepts laid down by the model. <ref>earthstudies.co.uk</ref> | ||
==References== | ==References== |
Revision as of 09:47, 22 May 2015
This article relies largely or entirely on a single source. Relevant discussion may be found on the talk page. Please help improve this article by introducing citations to additional sources. Find sources: "Bradshaw model" – news · newspapers · books · scholar · JSTOR (September 2012) |
The Bradshaw Model is a geographical model which describes how a river's characteristics vary between the upper course and lower course of a river. It shows that discharge, occupied channel width, channel depth and average load quantity increases downstream. Load le size, channel bed roughness and gradient are all characteristics that decrease; it is represented by triangles, of diffe rivers fit the model perfectly therefore the model is usually used in order to compare natural rivers to concepts laid down by the model.
References
- earthstudies.co.uk