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  • rainfall /3
  • rainfall /2
  • rainfall x2
  • uplift /2
  • uplift x2
  • uplift x3
  • grain size /10
  • grain size x5
  • Hillslope erodibility x10
  • Hillslope erodibility x100
  • Hillslope erodibility x1000
  • bank erosion
  • bank erosion x2
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Branching river network (experts)

  • Post published:10th April 2020
  • Post category:Experts

For experts. All the following equations and parameters are described in the Theory page. Why rivers networks have many branches or not? If we compare the simulations of this site…

Continue ReadingBranching river network (experts)

The transport capacity (experts)

  • Post published:25th March 2020
  • Post category:Experts

For the experts. All the following equations and parameters are described in the Theory page. Erosion and sedimentation in a river can be seen as resulting from the difference between…

Continue ReadingThe transport capacity (experts)

Equivalence of some parameters (experts)

  • Post published:24th March 2020
  • Post category:Experts

For the experts. All the following equations and parameters are described in the Theory page. Intuitively, decreasing the uplift rate may be equivalent to increasing the rainfall rate in terms…

Continue ReadingEquivalence of some parameters (experts)
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Guidelines for teaching

  • Branching river network (experts)
  • Unrealistic mountain height (beginners)
  • Stationarity of mean erosion rate but topography still moving (beginners)
  • The transport capacity (experts)
  • Equivalence of some parameters (experts)
  • Defying our intuition (beginners)
  • The scaling of mountain relief with rainfall (experts)
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