Table 2 Modeling characteristics of 1D and 2D in HEC-RAS for datasets 1 and 2.

From: Multidimensional Datasets Supporting Vulnerability Assessments of Riverine Bridges in Peru

Characteristics

HEC-RAS 1D

HEC-RAS 2D

Data set 1 (1D)

Data set 2 (1D)

Data set 2 (2D)

Mathematical formulation

1D Saint-Venant equations (continuity and momentum).

2D Saint-Venant equations (shallow water equations).

Continuity and momentum

Continuity and momentum

SWE-EM (Stricter Momentum)

Main dependent variable

Discharge Q(x,t) and water depth h(x,t).

Water depth h(x,y,t) and velocities \(u\) (x,y,t), \(\upsilon \) (x,y,t)

Steady flow with discharges of T = 100 (247.5 m³/s), T = 140 (259.3), T = 200 (271.5 m³/s) and T = 500 (301.9 m³/s) years.

Steady flow with discharges of T = 50 (223 m³/s), T = 100 (248.5 m³/s), T = 200 (273 m³/s) and T = 500 (304.3 m³/s) years

Unsteady flow for discharges of T = 50, T = 100, T = 200, and T = 500 years

Flow direction

Flow restricted to the longitudinal direction of the channel.

Free flow in two horizontal directions (x,y).

135 cross-sections

321 cross-sections perpendicular to the channel axis

Geometric representation

River profile through cross-sections perpendicular to the channel axis.

2D mesh that discretizes the entire floodplain.

9503 cells

Spacing DX = 5 m

Spacing DY = 5 m

Represented processes

Water levels and discharges along the channel axis. Handles structures (bridges).

Spatial flow dynamics: overflows, recirculation zones, floodplain flows.

Contraction coefficient (0.3), expansion (0.5), dredging (Cd = 1.33), and semicircular pier shape (K = 0.9)

Contraction coefficient (0.3), expansion (0.5), dredging (Cd = 1.33), and semicircular pier shape (K = 0.9)

Overflows, recirculation zones, floodplain flows

Boundary conditions

Defined at upstream and downstream cross-sections.

Defined at the upstream and downstream mesh boundaries.

Mixed flow (Normal Depth) for subcritical and supercritical flow

Mixed flow (Normal Depth) for subcritical and supercritical flow

Upstream and downstream (BClines)

Numerical resolution

Implicit finite difference scheme at discrete sections.

Finite volume method with conservative flow solution in cells.

Finite difference method (FDM)

Finite difference method (FDM)

Finite volume method (FVM)

Computational requirements

Low memory and computational time requirements.

High computational demand (depends on mesh size and refinement).

AMD Ryzen 7 5800H with Radeon Graphics

13th Gen Intel(R) Core (TM) i7-13650HX

AMD Ryzen 7 5800H with Radeon Graphics

Limitations

Does not adequately represent lateral flows, recirculations, or complex overflows.

High demand for topographic data and simulation times.

Discrete cross-section, linear, simplified floodplain

Discrete cross-section, linear, simplified floodplain

DTM (DJI Phantom 4 RTK drone, every meter) and time step based on Courant criterion (1 s)