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OpenSWMM Engine
6.0.0-alpha.4
Data-oriented, plugin-extensible SWMM Engine (6.0.0-alpha.4)
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Implementation of gradient computation, slope limiting, and edge fluxes. More...
#include "SurfaceFluxCalculator.hpp"#include "InertialKernels.hpp"#include "../data/BoundaryData.hpp"#include <cmath>#include <algorithm>#include <cstdlib>#include <limits>Namespaces | |
| namespace | openswmm |
| namespace | openswmm::twoD |
Functions | |
| void | openswmm::twoD::computeUnlimitedGradients (const MeshData &mesh, SurfaceStateData &state, int nthreads=1) |
| Compute unlimited gradients for all triangles via Green-Gauss theorem. | |
| void | openswmm::twoD::computeLimitedGradients (const MeshData &mesh, SurfaceStateData &state, double epsilon, int nthreads=1) |
| Apply Jawahar-Kamath slope limiter (Eq. [23]–[24]). | |
| void | openswmm::twoD::computeCellContinuity (const MeshData &mesh, SurfaceStateData &state, const SolverOptions2D &opts, double dt) |
| Compute the per-cell continuity residual (local mass-balance check). | |
| void | openswmm::twoD::computeFaceVelocity (const MeshData &mesh, SurfaceStateData &state, const SolverOptions2D &opts) |
| Reconstruct diagnostic cell velocity from wetted-edge normal velocities. | |
| double | openswmm::twoD::computeBoundaryEdgeFlux (const MeshData &mesh, const SurfaceStateData &state, const SolverOptions2D &opts, double dh_eps, int i, int idx) noexcept |
Boundary-edge flux for cell i across flat mesh edge slot idx (m³/s, inflow-positive). Exported wrapper over the file-local boundary kernel for host boundary queries. Explicit inertial marchers may use their own prognostic stage-boundary update instead. | |
| OPENSWMM_KERNEL_FN double | openswmm::twoD::faceDepthFromEta (double eta, double z_lo, double z_hi) noexcept |
| Wetted-edge flow depth from a free surface η over an edge with endpoint beds z_lo ≤ z_hi — Begnudelli & Sanders (2007) Eq. 14, the exact cross-sectional water area divided by the full edge length: η ≤ z_lo : 0 (wetting gate: bed above water) z_lo < η ≤ z_hi : (η − z_lo)² / (2(z_hi − z_lo)) (partially submerged) η > z_hi : η − (z_lo + z_hi)/2 (fully submerged: mean depth) The quadratic branch matches value AND slope at both joins (C¹), so overtopping onset is smooth. Single source for the CPU boundary path, the GPU boundary kernels, and the VFR interior-face path — byte-identical to the copies it replaced in SurfaceFluxCalculator.cpp and ExplicitKokkosSurfaceSolver.cpp. | |
Implementation of gradient computation, slope limiting, and edge fluxes.