Difference between revisions of "Segment"

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(General description)
(Segment)
 
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=Segment=
 
=Segment=
  
==General description==
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==Definition==
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Section of river subject to similar valley-scale influences and energy conditions.
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== Delineation criteria ==
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* Major changes in valley gradient
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* Major tributary confluences (significantly increasing upstream catchment area, river discharge)
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* Valley confinement (confined, partly-confined, unconfined)
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* In mountainous areas, very large lateral sediment inputs
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== Methods and data sources ==
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# Major segments are identified by applying GIS tools to a DEM with river network overlay, to define downstream breaks in valley gradient (and width) and in upstream contributing area.
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# Major segments may be subdivided according to valley confinement interpreted from DEMs
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# Google Earth images
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# Orthophotos
  
River segments are sections of the river network that are subjected to similar valley-scale influences and energy conditions. Delineation is based on major changes in valley gradient, major tributary confluences, and valley confinement.
 
  
 
<gallery>
 
<gallery>
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</gallery>
 
</gallery>
  
==Case studies where this River Characterisation is relevant==
 
  
<Forecasterlink type="getProjectsForRt" code="4"/>
 
==Tools where this River Characterisation is relevant==
 
  
<Forecasterlink type="getToolsForRt" code="4"/>
 
==Other relevant information==
 
  
 
  [[Category:River Characterisation]] [[Category:Segment]] [[Category:Segment]]
 
  [[Category:River Characterisation]] [[Category:Segment]] [[Category:Segment]]

Latest revision as of 13:58, 22 May 2014

Segment

Definition

Section of river subject to similar valley-scale influences and energy conditions.


Delineation criteria

  • Major changes in valley gradient
  • Major tributary confluences (significantly increasing upstream catchment area, river discharge)
  • Valley confinement (confined, partly-confined, unconfined)
  • In mountainous areas, very large lateral sediment inputs


Methods and data sources

  1. Major segments are identified by applying GIS tools to a DEM with river network overlay, to define downstream breaks in valley gradient (and width) and in upstream contributing area.
  2. Major segments may be subdivided according to valley confinement interpreted from DEMs
  3. Google Earth images
  4. Orthophotos