PISM, A Parallel Ice Sheet Model 2.2.2-d6b3a29ca committed by Constantine Khrulev on 2025-03-28
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◆ P_from_W_steady()
Compute functional relationship P(W) which applies only in steady state. In steady state in this model, water pressure is determined by a balance of cavitation (opening) caused by sliding and creep closure. This will be used in initialization when P is otherwise unknown, and in verification and/or reporting. It is not used during time-dependent model runs. To be more complete, P = P(W,P_o,|v_b|). Definition at line 170 of file Distributed.cc. References pism::Component::m_config, pism::Component::m_grid, and pism::Wr. Referenced by bootstrap_impl(). |