TaylorNonLinearDiffuser

Model non-linear soil creep

hillslopediffusion

true

Contributor(s)

Initial contribute: 2021-09-17

Authorship

:  
rachel.glade@colorado.edu
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Classification(s)

Application-focused categoriesNatural-perspectiveLand regions
Application-focused categoriesIntegrated-perspectiveRegional scale

Detailed Description

English {{currentDetailLanguage}} English

quoted from:https://csdms.colorado.edu/wiki/Model:TaylorNonLinearDiffuser

Hillslope evolution using a Taylor Series expansion of the Andrews-Bucknam formulation of nonlinear hillslope flux derived following following Ganti et al., 2012. The flux is given as:

qs = KS ( 1 + (S/Sc)**2 + (S / Sc)**4 + .. + (S / Sc)**2(n - 1) )

where K is is the diffusivity, S is the slope, Sc is the critical slope, and n is the number of terms. The default behavior uses two terms to produce a flux law as described by Equation 6 of Ganti et al., (2012).

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Rachel Glade (2021). TaylorNonLinearDiffuser, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/de4727e2-683d-4173-9f64-935a19a53c41
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Contributor(s)

Initial contribute : 2021-09-17

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Authorship

:  
rachel.glade@colorado.edu
Is authorship not correct? Feed back

History

Last modify time
2021-09-17

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