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solvers:temperature [2013/03/08 05:00] gag [SIF contents] |
solvers:temperature [2018/10/28 14:28] tzwinger [Examples] |
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The volumetric heat source term can be estimated from the ice flow deformational heat using the [[: | The volumetric heat source term can be estimated from the ice flow deformational heat using the [[: | ||
+ | |||
+ | **Looping option, added 6th June 2013 (version 6205)**: It is possible in some cases that the nonlinear convergence tolerance can be reached before all nodes have been properly constrained. | ||
+ | < | ||
+ | Loop While Unconstrained Nodes = Logical True | ||
+ | </ | ||
==== Known bugs ==== | ==== Known bugs ==== | ||
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! Units : MPa - m - yr | ! Units : MPa - m - yr | ||
$yearinsec = 365.25*24*60*60 | $yearinsec = 365.25*24*60*60 | ||
- | |||
!Compute the heat generated by ice deformation | !Compute the heat generated by ice deformation | ||
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Temp Flux BC = Logical True | Temp Flux BC = Logical True | ||
Temp Heat Flux = Real $56.05E-03*yearinsec*1.0E-6 | Temp Heat Flux = Real $56.05E-03*yearinsec*1.0E-6 | ||
+ | !------------------- | ||
+ | ! frictional heat | ||
+ | !-------------------- | ||
+ | Temp Load = Variable Velocity 1 | ||
+ | Real Procedure | ||
End | End | ||
</ | </ | ||
+ | |||
+ | See also [[: | ||
==== Examples ==== | ==== Examples ==== | ||
- | Download an example | + | An example |
==== Reference ==== | ==== Reference ==== | ||
When used this solver can be cited using the following reference: | When used this solver can be cited using the following reference: | ||
Zwinger T. , R. Greve, O. Gagliardini , T. Shiraiwa and M. Lyly, 2007. A full Stokes-flow thermo-mechanical model for firn and ice applied to the Gorshkov crater glacier, Kamchatka. Annals of Glaciol., 45, p. 29-37. | Zwinger T. , R. Greve, O. Gagliardini , T. Shiraiwa and M. Lyly, 2007. A full Stokes-flow thermo-mechanical model for firn and ice applied to the Gorshkov crater glacier, Kamchatka. Annals of Glaciol., 45, p. 29-37. |