PISM, A Parallel Ice Sheet Model 2.2.2-d6b3a29ca committed by Constantine Khrulev on 2025-03-28
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◆ ice_flow_rate_across_grounding_line()
Compute the ice flow rate across the grounding line, adding to When Negative flux corresponds to ice moving into the ocean, i.e. from grounded to floating areas. (This convention makes it easier to compare this quantity to the surface mass balance or calving fluxes.) Different choices of the
Compute the ice flow rate across the grounding line over a time step, adding to The units of Negative flux corresponds to ice moving into the ocean, i.e. from grounded to floating areas. (This convention makes it easier to compare this quantity to the surface mass balance or calving fluxes.) Definition at line 1262 of file GeometryEvolution.cc. References pism::ParallelSection::check(), pism::ParallelSection::failed(), pism::array::Array::grid(), pism::array::CellType::ocean(), pism::array::Staggered1::star(), pism::array::CellType1::star_int(), and volume_flow_rate_from_land_to_water(). Referenced by pism::diagnostics::GroundingLineFlux::update_impl(), and pism::diagnostics::MassTransportAcrossGroundingLine::update_impl(). |