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topography_drunken_sailor

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All of the approaches to free surface simulations (pseudo-free-surface formulation, 'stick air' approximation, ALE scheme) have been subject to an instability which has been termed a ‘‘sloshing,” or ‘‘drunken sailor effect” instability (Kaus et al., 2010).

This instability is arisen from the large density contrast typical at a free surface (surface or air-rock interface), compared with the much smaller internal density contrasts, severely limits the maximum stable timestep for free surface computations (Rose et al., 2017).

Test Model

Case 1: stick-air model

The model tested here is from case 2 in (Crameri et al., 2012). 4 cases are tested and used the same time interval (fixed to 5k years), solver ("mumps" with penalty = 1e6). (1) "stick air" with air density = 0 kg/m^3 (2) with water density = 1000 kg/m^3 (3) air density and remove the reference density (4) water density and remove the reference density (5) denser density = 3000 kg/m^3 (6) gradually changed density ( 3300 - 1 kg/m^3 within H = 50 km)

It turns out removing reference density can get the same results as not removing ones if doing the appropriate scaling. And comparing with air density, the water density model doesn't improve the stability a lot and will have a higher topography.

Case 2: Rayleigh-Taylor instability

The model tested here is from case 2 in (Kaus et al., 2010).

Case 3: Convergence model

The model tested here is a convergence model modified from (Erdős, Huismans & van der Beek, 2015).

Which added a stick air layer and the in-out flow is balance by the velocity of the rock part.

Related issue

Issue #363 in uw2

Issue #207 in uwg

Solution (maybe)

Reference

  • Crameri, F., Schmeling, H., Golabek, G. J., Duretz, T., Orendt, R., Buiter, S. J. H., ... & Tackley, P. J. (2012). A comparison of numerical surface topography calculations in geodynamic modelling: an evaluation of the ‘sticky air’method. Geophysical Journal International, 189(1), 38-54.
  • Kaus, B. J., Mühlhaus, H., & May, D. A. (2010). A stabilization algorithm for geodynamic numerical simulations with a free surface. Physics of the Earth and Planetary Interiors, 181(1-2), 12-20.
  • Rose, I., Buffett, B., & Heister, T. (2017). Stability and accuracy of free surface time integration in viscous flows. Physics of the Earth and Planetary Interiors, 262, 90-100.
  • Erdős, Z., Huismans, R. S., & van der Beek, P. (2015). First‐order control of syntectonic sedimentation on crustal‐scale structure of mountain belts. Journal of Geophysical Research: Solid Earth, 120(7), 5362-5377.

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Some models for testing “drunken sailor" instability

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