PISM, A Parallel Ice Sheet Model
stable v2.1.1 committed by Constantine Khrulev on 2024-12-04 13:36:58 -0900
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#include <cassert>
#include "pism/hydrology/Routing.hh"
#include "pism/util/array/CellType.hh"
#include "pism/util/error_handling.hh"
#include "pism/util/pism_utilities.hh"
#include "pism/util/Vars.hh"
#include "pism/geometry/Geometry.hh"
#include "pism/util/Profiling.hh"
#include "pism/util/Context.hh"
Go to the source code of this file.
Classes | |
class | pism::hydrology::diagnostics::BasalWaterPressure |
Reports the pressure of the transportable water in the subglacial layer. More... | |
class | pism::hydrology::diagnostics::RelativeBasalWaterPressure |
Reports the pressure of the transportable water in the subglacial layer as a fraction of the overburden pressure. More... | |
class | pism::hydrology::diagnostics::EffectiveBasalWaterPressure |
Reports the effective pressure of the transportable water in the subglacial layer, that is, the overburden pressure minus the pressure. More... | |
class | pism::hydrology::diagnostics::WallMelt |
Report the wall melt rate from dissipation of the potential energy of the transportable water. More... | |
class | pism::hydrology::diagnostics::BasalWaterVelocity |
Diagnostically reports the staggered-grid components of the velocity of the water in the subglacial layer. More... | |
class | pism::hydrology::diagnostics::HydraulicPotential |
Report hydraulic potential in the subglacial hydrology system. More... | |
Namespaces | |
pism | |
pism::hydrology | |
Sub-glacial hydrology models and related diagnostics. | |
pism::hydrology::diagnostics | |
Functions | |
void | pism::hydrology::diagnostics::hydraulic_potential (const array::Scalar &W, const array::Scalar &P, const array::Scalar &sea_level, const array::Scalar &bed, const array::Scalar &ice_thickness, array::Scalar &result) |
Compute the hydraulic potential. More... | |
void | pism::hydrology::wall_melt (const Routing &model, const array::Scalar &bed_elevation, array::Scalar &result) |
Compute the wall melt rate which comes from (turbulent) dissipation of flow energy. More... | |