Suggestion: md.friction.coupling uses md.initialization.hyraulic_potential
#109
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Hi @inwoo-park this is a good idea but I wonder if we are not reaching the limits of what Cheers |
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I agree that adding an additional Best regards, |
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Dear ISSM developers,
Suggestion
I would like to suggest an additional copuling method in
md.friction.coupling=5which usesmd.initialization.hydraulic_potential. Now, I try to use the effective pressure outputs from other external subglacial hydrology model that not implemented in ISSM. (specifically, the CUAS-MPI model: https://github.com/tudasc/CUAS-MPI)When using the$N_{\mathrm{eff}}$ throughout the entire simulation. This approach creates a limitation because it does not account for time-varying ice pressure ($\rho_i g H$ ). For example, the Budd-type friction law:
md.friction.coupling=3for the transient simulation (or projection), the model applies a fixed effective pressurewhere$N_{\rm{eff}} = \rho_i g H - P_w$ ($P_w$ is the water pressure). With
md.friction.coupling=3, the effective pressure remains contant withmd.friction.effecvtive_pressureduring the transient period.Therefore, I propose adding a new option,
md.friction.coupling=5with the following scheme:md.friction.effective_pressureCODE
The effective pressure calculated from
md.initialization.hyraulic_potentialmay be computed as:where$z_b$ is the base elevation of ice (
md.geometry.base)Then the effective pressure$N_{\mathrm{eff}}$ can be computed as:
ensuring that
negative the effective pressure is not allowed.I have created a branch
hydrology-couplinghere:GitHub - inwoo-park/ISSM at hydrology-coupling.
Would it be appropriate to submit the
hydrology-couplingbranch to theISSM/mainbranch?Best regards,
Inwoo
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