bootstrap_impl check_P_bounds define_model_state_impl Distributed init_impl initialization_message m_P m_Pnew max_timestep_P_diff P_from_W_steady restart_impl subglacial_water_pressure ts_diagnostics_impl update_impl update_P write_model_state_impl ~Distributed

P_from_W_steady() void pism::hydrology::Distributed::P_from_W_steady ( const array::Scalar &  W, const array::Scalar &  P_overburden, const array::Scalar &  sliding_speed, array::Scalar &  result  ) protected 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, pism::array::max(), and pism::Wr. Referenced by bootstrap_impl().