#include <SurfaceStateData.hpp>
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| const BoundaryData * | boundary = nullptr |
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| const NodeData * | nodes_1d = nullptr |
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| const std::vector< double > * | node_row_conc = nullptr |
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| const std::vector< CouplingPoint > * | node_coupling = nullptr |
| | non-outfall points
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| SurfaceTransportState | transport |
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| std::vector< double > | depth |
| | Mean wetted depth h̄ = V/A_wet (m) [reconstructed].
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| std::vector< double > | head |
| | Free-surface elevation η (m) [reconstructed].
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| std::vector< double > | volume |
| | Cell water volume V (m³) — the integrated state.
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| std::vector< double > | grad_hx |
| | ∂h/∂x (unlimited gradient)
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| std::vector< double > | grad_hy |
| | ∂h/∂y (unlimited gradient)
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| std::vector< double > | grad_hx_lim |
| | Limited gradient X.
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| std::vector< double > | grad_hy_lim |
| | Limited gradient Y.
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| std::vector< double > | vert_head |
| | Head reconstructed at vertices.
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| std::vector< double > | vert_depth_signed |
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| std::vector< double > | face_vx |
| | Cell velocity X component (m/s)
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| std::vector< double > | face_vy |
| | Cell velocity Y component (m/s)
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| std::vector< double > | cell_continuity_err |
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| std::vector< double > | edge_flux |
| | Normal flux through each edge.
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| std::vector< double > | rainfall |
| | Rainfall intensity (m/s)
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| std::vector< double > | evap_rate |
| | Evaporation demand rate (m/s, >= 0)
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| std::vector< double > | infil_rate |
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| std::vector< double > | infil_applied |
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| std::vector< double > | coupling_flux |
| | Exchange with SWMM node (m/s, + = into 2D)
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| std::vector< double > | coupling_applied |
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| std::vector< double > | net_source |
| | Net source/sink per cell (m/s)
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| std::vector< int8_t > | rainfall_forced |
| | 0=computed, 1=override, 2=add
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| std::vector< int8_t > | rainfall_persist |
| | 0=reset, 1=persist
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| std::vector< double > | rainfall_force_val |
| | Forced rainfall value.
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| std::vector< int8_t > | evap_forced |
| | 0=computed, 1=override, 2=add
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| std::vector< int8_t > | evap_persist |
| | 0=reset, 1=persist
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| std::vector< double > | evap_force_val |
| | Forced evaporation value.
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| std::vector< int8_t > | coupling_forced |
| | 0=computed, 1=override, 2=add
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| std::vector< int8_t > | coupling_persist |
| | 0=reset, 1=persist
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| std::vector< double > | coupling_force_val |
| | Forced coupling value.
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| bool | forcing_dirty = false |
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| bool | forcing_ever_set = false |
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| std::vector< double > | old_depth |
| | Mean depth at start of coupling interval.
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| std::vector< double > | old_volume |
| | Volume at start of coupling interval (m³)
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| std::vector< double > | stat_max_depth |
| | Maximum depth ψ_o seen at each cell (m)
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| std::vector< double > | stat_max_velocity |
| | Max cell speed |v| = √(vx²+vy²) (m/s)
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| std::vector< double > | stat_max_cont_err |
| | Max |cell_continuity_err| (m³/s)
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| std::vector< double > | stat_cum_volume |
| | Cumulative volume through cell (m³)
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| double | evap_loss_total = 0.0 |
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◆ clear_reset_forcings()
| void openswmm::twoD::SurfaceStateData::clear_reset_forcings |
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inlinenoexcept |
Clear RESET forcings after each step.
◆ reset_state()
| void openswmm::twoD::SurfaceStateData::reset_state |
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inlinenoexcept |
◆ resize()
| void openswmm::twoD::SurfaceStateData::resize |
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int | n_triangles, |
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int | n_vertices ) |
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inline |
◆ save_state()
| void openswmm::twoD::SurfaceStateData::save_state |
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inlinenoexcept |
◆ update_statistics()
| void openswmm::twoD::SurfaceStateData::update_statistics |
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const std::vector< double > & | tri_area, |
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double | dt, |
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int | nthreads = 1 ) |
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inlinenoexcept |
Update cumulative statistics / rendering envelopes.
Aggregates once per model (routing) step at the accepted end-of-step state. MUST be called after computeFaceVelocity and computeCellContinuity so face_vx/vy and cell_continuity_err hold the accepted values. All envelopes fuse into the single per-cell loop already walked for stat_cum_volume — no extra passes, no sub-step sampling.
◆ boundary
| const BoundaryData* openswmm::twoD::SurfaceStateData::boundary = nullptr |
Non-owning view of the per-edge boundary conditions (owned by SurfaceRouter2D). nullptr ⇒ all boundary edges are no-flux walls (the legacy behaviour, and what the unit-test call sites that build a bare state get). When set, computeEdgeFluxes applies the per-type boundary flux (NORMAL_FLOW / SPECIFIED_STAGE / SPECIFIED_FLOW / RATING_CURVE). The pointer is shallow-copied on assignment (it references config, not per-cell state), which is fine — both copies see the same BC config.
◆ cell_continuity_err
| std::vector<double> openswmm::twoD::SurfaceStateData::cell_continuity_err |
◆ coupling_applied
| std::vector<double> openswmm::twoD::SurfaceStateData::coupling_applied |
SIGNED per-cell coupling exchange VOLUME (m³) accumulated since the last mass-balance read, then zeroed by it. Positive = water arrived in this cell from the 1D node (spill / outfall discharge); negative = water was abstracted from this cell into the node (drain).
Signed on purpose, and per cell on purpose. The domain totals (MassBalance2D::coupling_1d_to_2d_in / coupling_2d_to_1d_out) are two unsigned accumulators and cannot answer "what did THIS cell give
or take", which is the question asked of a coupling point that flip-flops within a batch: the two directions cancel in the net and both are invisible in the totals. coupling_flux is a rate that is overwritten every step, so it cannot answer it either.
Booked at the SAME dt and the same share the marcher applied, exactly like infil_applied above and for the same reason — re-deriving it from end-of-step state is first-order and under-books the cells that dried mid-step.
◆ coupling_flux
| std::vector<double> openswmm::twoD::SurfaceStateData::coupling_flux |
Exchange with SWMM node (m/s, + = into 2D)
◆ coupling_force_val
| std::vector<double> openswmm::twoD::SurfaceStateData::coupling_force_val |
◆ coupling_forced
| std::vector<int8_t> openswmm::twoD::SurfaceStateData::coupling_forced |
0=computed, 1=override, 2=add
◆ coupling_persist
| std::vector<int8_t> openswmm::twoD::SurfaceStateData::coupling_persist |
◆ depth
| std::vector<double> openswmm::twoD::SurfaceStateData::depth |
Mean wetted depth h̄ = V/A_wet (m) [reconstructed].
◆ edge_flux
| std::vector<double> openswmm::twoD::SurfaceStateData::edge_flux |
Normal flux through each edge.
◆ evap_force_val
| std::vector<double> openswmm::twoD::SurfaceStateData::evap_force_val |
Forced evaporation value.
◆ evap_forced
| std::vector<int8_t> openswmm::twoD::SurfaceStateData::evap_forced |
0=computed, 1=override, 2=add
◆ evap_loss_total
| double openswmm::twoD::SurfaceStateData::evap_loss_total = 0.0 |
Cumulative evaporation loss over the whole simulation (m³). Kept here (not in core's MassBalance2D, owned by another work stream) and folded into the API-level totals by Api2D.cpp.
◆ evap_persist
| std::vector<int8_t> openswmm::twoD::SurfaceStateData::evap_persist |
◆ evap_rate
| std::vector<double> openswmm::twoD::SurfaceStateData::evap_rate |
Evaporation demand rate (m/s, >= 0)
◆ face_vx
| std::vector<double> openswmm::twoD::SurfaceStateData::face_vx |
Cell velocity X component (m/s)
◆ face_vy
| std::vector<double> openswmm::twoD::SurfaceStateData::face_vy |
Cell velocity Y component (m/s)
◆ forcing_dirty
| bool openswmm::twoD::SurfaceStateData::forcing_dirty = false |
Set by the forcing API and by clear_reset_forcings() when any flag changes; consumed by the co-advance to bypass its coarse (30 s) forcing-refresh cadence, so a one-shot (RESET) prescription applies on the very next step and expires on the step after — the per-step semantics the swmm_2d_force_* API documents.
◆ forcing_ever_set
| bool openswmm::twoD::SurfaceStateData::forcing_ever_set = false |
Sticky companion to forcing_dirty: set by the forcing API the first time any prescription is written, never cleared. clear_reset_forcings() is called once per routing step and is O(n_cells); on a model that never uses the forcing API (every deck without an external controller) the whole sweep is dead work, and this flag skips it.
◆ grad_hx
| std::vector<double> openswmm::twoD::SurfaceStateData::grad_hx |
∂h/∂x (unlimited gradient)
◆ grad_hx_lim
| std::vector<double> openswmm::twoD::SurfaceStateData::grad_hx_lim |
◆ grad_hy
| std::vector<double> openswmm::twoD::SurfaceStateData::grad_hy |
∂h/∂y (unlimited gradient)
◆ grad_hy_lim
| std::vector<double> openswmm::twoD::SurfaceStateData::grad_hy_lim |
◆ head
| std::vector<double> openswmm::twoD::SurfaceStateData::head |
Free-surface elevation η (m) [reconstructed].
◆ infil_applied
| std::vector<double> openswmm::twoD::SurfaceStateData::infil_applied |
Infiltration APPLIED depth (m) accumulated since the last mass-balance read, then zeroed by it. Every site that integrates the infiltration sink into volume adds infilSink(...) * dt here with the SAME depth and the SAME dt it used, so the ledger books what the marcher actually removed. Re-deriving the loss from the accepted end-of-step depth is only first-order: a cell that dries mid-step is sunk at the higher early-step rate but re-derived at the ramped end-of-step rate, and the lazy tier integrates a stale depth across a whole sync interval. Both leave storage falling by more than the ledger books.
◆ infil_rate
| std::vector<double> openswmm::twoD::SurfaceStateData::infil_rate |
Infiltration loss rate (m/s, >= 0) — a HELD rate (plan §5.5.2, D-I1): Infil2D::updateRates republishes it on the INFIL_STEP cadence and it is held constant in between, exactly as rainfall is. The marcher NEVER evaluates an infiltration kernel per substep; it only consumes this array through infilSink(), so infiltration has no interaction with the LTS tiering or active set. All-zero when no [2D_INFILTRATION*] rows resolved — the bitwise-regression fast path (gate I7).
◆ net_source
| std::vector<double> openswmm::twoD::SurfaceStateData::net_source |
Net source/sink per cell (m/s)
◆ node_coupling
| const std::vector<CouplingPoint>* openswmm::twoD::SurfaceStateData::node_coupling = nullptr |
◆ node_row_conc
| const std::vector<double>* openswmm::twoD::SurfaceStateData::node_row_conc = nullptr |
S4: the 1D nodes' PUBLISHED row values, [node * n_species + s] in the 2D transport row order (pollutant conc, MSX conc, age, temperature), assembled by the router before each advance and frozen for the batch. What a 1D→2D spill or outfall discharge arrives at.
◆ nodes_1d
| const NodeData* openswmm::twoD::SurfaceStateData::nodes_1d = nullptr |
Live node-coupling view, set by SurfaceRouter2D. The marcher evaluates the 1D↔2D orifice exchange per substep against the CURRENT 2D head (so it self-limits) and accumulates the exact ∫Q dt per point. nodes_1d is the 1D node data, frozen for the duration of the batch.
◆ old_depth
| std::vector<double> openswmm::twoD::SurfaceStateData::old_depth |
Mean depth at start of coupling interval.
◆ old_volume
| std::vector<double> openswmm::twoD::SurfaceStateData::old_volume |
Volume at start of coupling interval (m³)
◆ rainfall
| std::vector<double> openswmm::twoD::SurfaceStateData::rainfall |
◆ rainfall_force_val
| std::vector<double> openswmm::twoD::SurfaceStateData::rainfall_force_val |
◆ rainfall_forced
| std::vector<int8_t> openswmm::twoD::SurfaceStateData::rainfall_forced |
0=computed, 1=override, 2=add
◆ rainfall_persist
| std::vector<int8_t> openswmm::twoD::SurfaceStateData::rainfall_persist |
◆ stat_cum_volume
| std::vector<double> openswmm::twoD::SurfaceStateData::stat_cum_volume |
Cumulative volume through cell (m³)
◆ stat_max_cont_err
| std::vector<double> openswmm::twoD::SurfaceStateData::stat_max_cont_err |
Max |cell_continuity_err| (m³/s)
◆ stat_max_depth
| std::vector<double> openswmm::twoD::SurfaceStateData::stat_max_depth |
Maximum depth ψ_o seen at each cell (m)
◆ stat_max_velocity
| std::vector<double> openswmm::twoD::SurfaceStateData::stat_max_velocity |
Max cell speed |v| = √(vx²+vy²) (m/s)
◆ transport
S1 — overland species transport. transport.active() is false (and every marcher species branch is skipped) unless the router sized it, so a hydrodynamics-only model pays one predicate per firing and is otherwise untouched. Embedded rather than pointed-to: it is per-cell STATE, sized with volume, and it is copied when the state is.
◆ vert_depth_signed
| std::vector<double> openswmm::twoD::SurfaceStateData::vert_depth_signed |
Render/output-only SIGNED vertex depth η_v − z_v (m) — wet-masked, depth-weighted reconstruction (reconstructVertexRenderDepths). Unlike vert_head, dry-cell bed elevations never contribute, and a wet cell votes only where its η reaches the corner (wetted-contact gate), so this field is safe to interpolate for the water surface. Emitted values are strictly positive or the 0 no-data sentinel (no qualifying incident cell); negatives appear only in files from older engines — readers stay negative-tolerant. NOT used by the solver.
◆ vert_head
| std::vector<double> openswmm::twoD::SurfaceStateData::vert_head |
Head reconstructed at vertices.
◆ volume
| std::vector<double> openswmm::twoD::SurfaceStateData::volume |
Cell water volume V (m³) — the integrated state.
The documentation for this struct was generated from the following file: