1ccaff030SJeremy L Thompson## libCEED: Navier-Stokes Example 2ccaff030SJeremy L Thompson 3ccaff030SJeremy L ThompsonThis page provides a description of the Navier-Stokes example for the libCEED library, based on PETSc. 4ccaff030SJeremy L Thompson 5ccaff030SJeremy L ThompsonThe Navier-Stokes problem solves the compressible Navier-Stokes equations in three dimensions using an 6ccaff030SJeremy L Thompsonexplicit time integration. The state variables are mass density, momentum density, and energy density. 7ccaff030SJeremy L Thompson 8ccaff030SJeremy L ThompsonThe main Navier-Stokes solver for libCEED is defined in [`navierstokes.c`](navierstokes.c) 9ccaff030SJeremy L Thompsonwith different problem definitions according to the application of interest. 10ccaff030SJeremy L Thompson 11ccaff030SJeremy L ThompsonBuild by using 12ccaff030SJeremy L Thompson 13ccaff030SJeremy L Thompson`make` 14ccaff030SJeremy L Thompson 15ccaff030SJeremy L Thompsonand run with 16ccaff030SJeremy L Thompson 17ff6701fcSJed Brown`./navierstokes` 18ccaff030SJeremy L Thompson 19ccaff030SJeremy L ThompsonAvailable runtime options are: 20ccaff030SJeremy L Thompson 21ccaff030SJeremy L Thompson| Option | Meaning | 2281f92cf0SLeila Ghaffari| :-------------------------------------| :-----------------------------------------------------------------------------------------------| 23ccaff030SJeremy L Thompson| `-ceed` | CEED resource specifier | 24ccaff030SJeremy L Thompson| `-test` | Run in test mode | 25e43605a5SLeila Ghaffari| `-problem` | Problem to solve (`advection`, `advection2d`, `density_current`, or `euler_vortex`) | 2681f92cf0SLeila Ghaffari| `-problem_advection_wind` | Wind type in Advection (`rotation` or `translation`) | 2781f92cf0SLeila Ghaffari| `-problem_advection_wind_translation` | Constant wind vector when `-problem_advection_wind translation` | 28e43605a5SLeila Ghaffari| `-problem_euler_mean_velocity` | Constant mean velocity vector in `euler_vortex` | 29e43605a5SLeila Ghaffari| `-vortex_strength` | Strength of vortex in `euler_vortex` | 30ccaff030SJeremy L Thompson| `-stab` | Stabilization method | 31ccaff030SJeremy L Thompson| `-implicit` | Use implicit time integartor formulation | 32ccaff030SJeremy L Thompson| `-bc_wall` | Use wall boundary conditions on this list of faces | 33ccaff030SJeremy L Thompson| `-bc_slip_x` | Use slip boundary conditions, for the x component, on this list of faces | 34ccaff030SJeremy L Thompson| `-bc_slip_y` | Use slip boundary conditions, for the y component, on this list of faces | 35ccaff030SJeremy L Thompson| `-bc_slip_z` | Use slip boundary conditions, for the z component, on this list of faces | 36ccaff030SJeremy L Thompson| `-viz_refine` | Use regular refinement for visualization | 37ff6701fcSJed Brown| `-degree` | Polynomial degree of tensor product basis (must be >= 1) | 38ccaff030SJeremy L Thompson| `-units_meter` | 1 meter in scaled length units | 39ccaff030SJeremy L Thompson| `-units_second` | 1 second in scaled time units | 40ccaff030SJeremy L Thompson| `-units_kilogram` | 1 kilogram in scaled mass units | 41ccaff030SJeremy L Thompson| `-units_Kelvin` | 1 Kelvin in scaled temperature units | 42ccaff030SJeremy L Thompson| `-theta0` | Reference potential temperature | 43ccaff030SJeremy L Thompson| `-thetaC` | Perturbation of potential temperature | 44ccaff030SJeremy L Thompson| `-P0` | Atmospheric pressure | 4516c0476cSLeila Ghaffari| `-E_wind` | Total energy of inflow wind | 46ccaff030SJeremy L Thompson| `-N` | Brunt-Vaisala frequency | 47ccaff030SJeremy L Thompson| `-cv` | Heat capacity at constant volume | 48ccaff030SJeremy L Thompson| `-cp` | Heat capacity at constant pressure | 49ccaff030SJeremy L Thompson| `-g` | Gravitational acceleration | 50ccaff030SJeremy L Thompson| `-lambda` | Stokes hypothesis second viscosity coefficient | 51ccaff030SJeremy L Thompson| `-mu` | Shear dynamic viscosity coefficient | 52ccaff030SJeremy L Thompson| `-k` | Thermal conductivity | 53ccaff030SJeremy L Thompson| `-CtauS` | Scale coefficient for stabilization tau (nondimensional) | 54ccaff030SJeremy L Thompson| `-strong_form` | Strong (1) or weak/integrated by parts (0) advection residual | 55ccaff030SJeremy L Thompson| `-lx` | Length scale in x direction | 56ccaff030SJeremy L Thompson| `-ly` | Length scale in y direction | 57ccaff030SJeremy L Thompson| `-lz` | Length scale in z direction | 58ccaff030SJeremy L Thompson| `-rc` | Characteristic radius of thermal bubble | 59ccaff030SJeremy L Thompson| `-resx` | Resolution in x | 60ccaff030SJeremy L Thompson| `-resy` | Resolution in y | 61ccaff030SJeremy L Thompson| `-resz` | Resolution in z | 62ccaff030SJeremy L Thompson| `-center` | Location of bubble center | 63ccaff030SJeremy L Thompson| `-dc_axis` | Axis of density current cylindrical anomaly, or {0,0,0} for spherically symmetric | 64ccaff030SJeremy L Thompson| `-output_freq` | Frequency of output, in number of steps | 65ccaff030SJeremy L Thompson| `-continue` | Continue from previous solution | 66ccaff030SJeremy L Thompson| `-degree` | Polynomial degree of tensor product basis | 67ccaff030SJeremy L Thompson| `-qextra` | Number of extra quadrature points | 6881f92cf0SLeila Ghaffari| `-qextra_boundary` | Number of extra quadrature points on in/outflow faces | 69d99129b9SLeila Ghaffari| `-output_dir` | Output directory | 70ccaff030SJeremy L Thompson 71c063f476SvaleriabarraFor the case of a square/cubic mesh, the list of face indices to be used with `-bc_wall` and/or `-bc_slip_x`, 72ed1c75c9SLeila Ghaffari`-bc_slip_y`, and `-bc_slip_z` are: 73c063f476Svaleriabarra 74c063f476Svaleriabarra* 2D: 75c063f476Svaleriabarra - faceMarkerBottom = 1; 76c063f476Svaleriabarra - faceMarkerRight = 2; 77c063f476Svaleriabarra - faceMarkerTop = 3; 78c063f476Svaleriabarra - faceMarkerLeft = 4; 79c063f476Svaleriabarra* 3D: 80c063f476Svaleriabarra - faceMarkerBottom = 1; 81c063f476Svaleriabarra - faceMarkerTop = 2; 82c063f476Svaleriabarra - faceMarkerFront = 3; 83c063f476Svaleriabarra - faceMarkerBack = 4; 84c063f476Svaleriabarra - faceMarkerRight = 5; 85c063f476Svaleriabarra - faceMarkerLeft = 6; 86ccaff030SJeremy L Thompson 87ccaff030SJeremy L Thompson### Advection 88ccaff030SJeremy L Thompson 89ccaff030SJeremy L ThompsonThis problem solves the convection (advection) equation for the total (scalar) energy density, 90ccaff030SJeremy L Thompsontransported by the (vector) velocity field. 91ccaff030SJeremy L Thompson 92ccaff030SJeremy L ThompsonThis is 3D advection given in two formulations based upon the weak form. 93ccaff030SJeremy L Thompson 94ccaff030SJeremy L ThompsonState Variables: 95ccaff030SJeremy L Thompson 96ccaff030SJeremy L Thompson *q = ( rho, U<sub>1</sub>, U<sub>2</sub>, U<sub>3</sub>, E )* 97ccaff030SJeremy L Thompson 98ccaff030SJeremy L Thompson *rho* - Mass Density 99ccaff030SJeremy L Thompson 100ccaff030SJeremy L Thompson *U<sub>i</sub>* - Momentum Density , *U<sub>i</sub> = rho ui* 101ccaff030SJeremy L Thompson 102ccaff030SJeremy L Thompson *E* - Total Energy Density, *E = rho Cv T + rho (u u) / 2 + rho g z* 103ccaff030SJeremy L Thompson 104ccaff030SJeremy L ThompsonAdvection Equation: 105ccaff030SJeremy L Thompson 106ccaff030SJeremy L Thompson *dE/dt + div( E _u_ ) = 0* 107ccaff030SJeremy L Thompson 108ccaff030SJeremy L Thompson#### Initial Conditions 109ccaff030SJeremy L Thompson 110ccaff030SJeremy L ThompsonMass Density: 111ccaff030SJeremy L Thompson Constant mass density of 1.0 112ccaff030SJeremy L Thompson 113ccaff030SJeremy L ThompsonMomentum Density: 114ccaff030SJeremy L Thompson Rotational field in x,y with no momentum in z 115ccaff030SJeremy L Thompson 116ccaff030SJeremy L ThompsonEnergy Density: 117ccaff030SJeremy L Thompson Maximum of 1. x0 decreasing linearly to 0. as radial distance increases 118ccaff030SJeremy L Thompson to 1/8, then 0. everywhere else 119ccaff030SJeremy L Thompson 120ccaff030SJeremy L Thompson#### Boundary Conditions 121ccaff030SJeremy L Thompson 122*89d0f5c0SLeila GhaffariThis problem is solved for two test cases with different BCs. 123*89d0f5c0SLeila Ghaffari 124*89d0f5c0SLeila Ghaffari##### Rotation 125*89d0f5c0SLeila Ghaffari 126ccaff030SJeremy L ThompsonMass Density: 127ccaff030SJeremy L Thompson 0.0 flux 128ccaff030SJeremy L Thompson 129ccaff030SJeremy L ThompsonMomentum Density: 130ccaff030SJeremy L Thompson 0.0 131ccaff030SJeremy L Thompson 132ccaff030SJeremy L ThompsonEnergy Density: 133ccaff030SJeremy L Thompson 0.0 flux 134ccaff030SJeremy L Thompson 135*89d0f5c0SLeila Ghaffari##### Translation 136*89d0f5c0SLeila Ghaffari 137*89d0f5c0SLeila GhaffariMass Density: 138*89d0f5c0SLeila Ghaffari 0.0 flux 139*89d0f5c0SLeila Ghaffari 140*89d0f5c0SLeila GhaffariMomentum Density: 141*89d0f5c0SLeila Ghaffari 0.0 142*89d0f5c0SLeila Ghaffari 143*89d0f5c0SLeila GhaffariEnergy Density: 144*89d0f5c0SLeila Ghaffari 145*89d0f5c0SLeila GhaffariInflow BCs: 146*89d0f5c0SLeila Ghaffari *E = E</sub>wind</sub>* 147*89d0f5c0SLeila Ghaffari 148*89d0f5c0SLeila GhaffariOutflow BCs: 149*89d0f5c0SLeila Ghaffari *E = E</sub>boundary</sub>* 150*89d0f5c0SLeila Ghaffari 151*89d0f5c0SLeila GhaffariBoth In/Outflow BCs for E are applied weakly. 152*89d0f5c0SLeila Ghaffari 153*89d0f5c0SLeila Ghaffari 154e43605a5SLeila Ghaffari### Euler Traveling Vortex 155e43605a5SLeila Ghaffari 156e43605a5SLeila GhaffariThis problem solves the 3D Euler equations for vortex evolution provided 157e43605a5SLeila Ghaffariin On the Order of Accuracy and Numerical Performance of Two Classes of 158e43605a5SLeila GhaffariFinite Volume WENO Schemes, Zhang, Zhang, and Shu (2011). 159e43605a5SLeila Ghaffari 160e43605a5SLeila GhaffariState Variables: 161e43605a5SLeila Ghaffari 162e43605a5SLeila Ghaffari *q = ( rho, U<sub>1</sub>, U<sub>2</sub>, U<sub>3</sub>, E )* 163e43605a5SLeila Ghaffari 164e43605a5SLeila Ghaffari *rho* - Mass Density 165e43605a5SLeila Ghaffari 166e43605a5SLeila Ghaffari *U<sub>i</sub>* - Momentum Density , *U<sub>i</sub> = rho u<sub>i</sub>* 167e43605a5SLeila Ghaffari 168e43605a5SLeila Ghaffari *E* - Total Energy Density, *E = P / (gamma - 1) + rho (u u) / 2* 169e43605a5SLeila Ghaffari 170e43605a5SLeila GhaffariEuler Equations: 171e43605a5SLeila Ghaffari 172e43605a5SLeila Ghaffari *drho/dt + div( U ) = 0* 173e43605a5SLeila Ghaffari 174e43605a5SLeila Ghaffari *dU/dt + div( rho (u x u) + P I<sub>3</sub> ) = 0* 175e43605a5SLeila Ghaffari 176e43605a5SLeila Ghaffari *dE/dt + div( (E + P) u ) = 0* 177e43605a5SLeila Ghaffari 178e43605a5SLeila GhaffariConstants: 179e43605a5SLeila Ghaffari 180e43605a5SLeila Ghaffari *c<sub>v</sub>* , Specific heat, constant volume 181e43605a5SLeila Ghaffari 182e43605a5SLeila Ghaffari *c<sub>p</sub>* , Specific heat, constant pressure 183e43605a5SLeila Ghaffari 184e43605a5SLeila Ghaffari *gamma = c<sub>p</sub> / c<sub>v</sub>*, Specific heat ratio 185e43605a5SLeila Ghaffari 186e43605a5SLeila Ghaffari *epsilon* , Vortex Strength 187e43605a5SLeila Ghaffari 188e43605a5SLeila Ghaffari#### Initial Conditions 189e43605a5SLeila Ghaffari 190e43605a5SLeila GhaffariTemperature: 191e43605a5SLeila Ghaffari 192e43605a5SLeila Ghaffari *T = 1 - (gamma - 1) epsilon^2 exp(1 - r^2) / (8 gamma pi^2)* 193e43605a5SLeila Ghaffari 194e43605a5SLeila GhaffariEntropy: 195e43605a5SLeila Ghaffari 196e43605a5SLeila Ghaffari *S = 1* , Constant entropy 197e43605a5SLeila Ghaffari 198e43605a5SLeila GhaffariDensity: 199e43605a5SLeila Ghaffari 200e43605a5SLeila Ghaffari *rho = (T/S)^(1 / (gamma - 1))* 201e43605a5SLeila Ghaffari 202e43605a5SLeila GhaffariPressure: 203e43605a5SLeila Ghaffari 204e43605a5SLeila Ghaffari *P = rho T* 205e43605a5SLeila Ghaffari 206e43605a5SLeila GhaffariVelocity: 207e43605a5SLeila Ghaffari 208e43605a5SLeila Ghaffari *u<sub>i</sub> = 1 + epsilon exp((1 - r^2)/2) [yc - y, x - xc, 0] / (2 pi)* 209e43605a5SLeila Ghaffari 210e43605a5SLeila Ghaffari *r = sqrt( (x - xc)^2 + (y - yc)^2 )* 211e43605a5SLeila Ghaffari with *(xc,yc)* center of the xy-plane in the domain 212e43605a5SLeila Ghaffari 213e43605a5SLeila Ghaffari#### Boundary Conditions 214e43605a5SLeila Ghaffari 215e43605a5SLeila GhaffariFor this problem, in/outflow BCs are implemented where the validity of the weak 216e43605a5SLeila Ghaffariform of the governing equations is extended to the outflow. 217e43605a5SLeila GhaffariFor the inflow fluxes, prescribed T_inlet and P_inlet are converted to 218e43605a5SLeila Ghaffariconservative variables and applied weakly. 219e43605a5SLeila Ghaffari 220ccaff030SJeremy L Thompson### Density Current 221ccaff030SJeremy L Thompson 222ccaff030SJeremy L ThompsonThis problem solves the full compressible Navier-Stokes equations, using 223ccaff030SJeremy L Thompsonoperator composition and design of coupled solvers in the context of atmospheric 224ccaff030SJeremy L Thompsonmodeling. This problem uses the formulation given in Semi-Implicit Formulations 225ccaff030SJeremy L Thompsonof the Navier-Stokes Equations: Application to Nonhydrostatic Atmospheric Modeling, 226ccaff030SJeremy L ThompsonGiraldo, Restelli, and Lauter (2010). 227ccaff030SJeremy L Thompson 228ccaff030SJeremy L ThompsonThe 3D compressible Navier-Stokes equations are formulated in conservation form with state 229ccaff030SJeremy L Thompsonvariables of density, momentum density, and total energy density. 230ccaff030SJeremy L Thompson 231ccaff030SJeremy L ThompsonState Variables: 232ccaff030SJeremy L Thompson 233ccaff030SJeremy L Thompson *q = ( rho, U<sub>1</sub>, U<sub>2</sub>, U<sub>3</sub>, E )* 234ccaff030SJeremy L Thompson 235ccaff030SJeremy L Thompson *rho* - Mass Density 236ccaff030SJeremy L Thompson 237ccaff030SJeremy L Thompson *U<sub>i</sub>* - Momentum Density , *U<sub>i</sub> = rho u<sub>i</sub>* 238ccaff030SJeremy L Thompson 239ccaff030SJeremy L Thompson *E* - Total Energy Density, *E = rho c<sub>v</sub> T + rho (u u) / 2 + rho g z* 240ccaff030SJeremy L Thompson 241ccaff030SJeremy L ThompsonNavier-Stokes Equations: 242ccaff030SJeremy L Thompson 243ccaff030SJeremy L Thompson *drho/dt + div( U ) = 0* 244ccaff030SJeremy L Thompson 245ccaff030SJeremy L Thompson *dU/dt + div( rho (u x u) + P I<sub>3</sub> ) + rho g khat = div( F<sub>u</sub> )* 246ccaff030SJeremy L Thompson 247ccaff030SJeremy L Thompson *dE/dt + div( (E + P) u ) = div( F<sub>e</sub> )* 248ccaff030SJeremy L Thompson 249ccaff030SJeremy L ThompsonViscous Stress: 250ccaff030SJeremy L Thompson 251ccaff030SJeremy L Thompson *F<sub>u</sub> = mu (grad( u ) + grad( u )^T + lambda div ( u ) I<sub>3</sub>)* 252ccaff030SJeremy L Thompson 253ccaff030SJeremy L ThompsonThermal Stress: 254ccaff030SJeremy L Thompson 255ccaff030SJeremy L Thompson *F<sub>e</sub> = u F<sub>u</sub> + k grad( T )* 256ccaff030SJeremy L Thompson 257ccaff030SJeremy L ThompsonEquation of State: 258ccaff030SJeremy L Thompson 259ccaff030SJeremy L Thompson *P = (gamma - 1) (E - rho (u u) / 2 - rho g z)* 260ccaff030SJeremy L Thompson 261ccaff030SJeremy L ThompsonTemperature: 262ccaff030SJeremy L Thompson 263ccaff030SJeremy L Thompson *T = (E / rho - (u u) / 2 - g z) / c<sub>v</sub>* 264ccaff030SJeremy L Thompson 265ccaff030SJeremy L ThompsonConstants: 266ccaff030SJeremy L Thompson 267ccaff030SJeremy L Thompson *lambda = - 2 / 3*, From Stokes hypothesis 268ccaff030SJeremy L Thompson 269ccaff030SJeremy L Thompson *mu* , Dynamic viscosity 270ccaff030SJeremy L Thompson 271ccaff030SJeremy L Thompson *k* , Thermal conductivity 272ccaff030SJeremy L Thompson 273ccaff030SJeremy L Thompson *c<sub>v</sub>* , Specific heat, constant volume 274ccaff030SJeremy L Thompson 275ccaff030SJeremy L Thompson *c<sub>p</sub>* , Specific heat, constant pressure 276ccaff030SJeremy L Thompson 277ccaff030SJeremy L Thompson *g* , Gravity 278ccaff030SJeremy L Thompson 279ccaff030SJeremy L Thompson *gamma = c<sub>p</sub> / c<sub>v</sub>*, Specific heat ratio 280ccaff030SJeremy L Thompson 281ccaff030SJeremy L Thompson#### Initial Conditions 282ccaff030SJeremy L Thompson 283ccaff030SJeremy L ThompsonPotential Temperature: 284ccaff030SJeremy L Thompson 285ccaff030SJeremy L Thompson *theta = thetabar + deltatheta* 286ccaff030SJeremy L Thompson 287ccaff030SJeremy L Thompson *thetabar = theta0 exp( N * * 2 z / g )* 288ccaff030SJeremy L Thompson 289ccaff030SJeremy L Thompson *deltatheta = 290ccaff030SJeremy L Thompson r <= rc : theta0(1 + cos(pi r)) / 2 291ccaff030SJeremy L Thompson r > rc : 0* 292ccaff030SJeremy L Thompson 293ccaff030SJeremy L Thompson *r = sqrt( (x - xc) * * 2 + (y - yc) * * 2 + (z - zc) * * 2 )* 294ccaff030SJeremy L Thompson with *(xc,yc,zc)* center of domain 295ccaff030SJeremy L Thompson 296ccaff030SJeremy L ThompsonExner Pressure: 297ccaff030SJeremy L Thompson 298ccaff030SJeremy L Thompson *Pi = Pibar + deltaPi* 299ccaff030SJeremy L Thompson 300ccaff030SJeremy L Thompson *Pibar = g * * 2 (exp( - N * * 2 z / g ) - 1) / (cp theta0 N * * 2)* 301ccaff030SJeremy L Thompson 302ccaff030SJeremy L Thompson *deltaPi = 0* (hydrostatic balance) 303ccaff030SJeremy L Thompson 304ccaff030SJeremy L ThompsonVelocity/Momentum Density: 305ccaff030SJeremy L Thompson 306ccaff030SJeremy L Thompson *U<sub>i</sub> = u<sub>i</sub> = 0* 307ccaff030SJeremy L Thompson 308ccaff030SJeremy L ThompsonConversion to Conserved Variables: 309ccaff030SJeremy L Thompson 310ccaff030SJeremy L Thompson *rho = P0 Pi**(c<sub>v</sub>/R<sub>d</sub>) / (R<sub>d</sub> theta)* 311ccaff030SJeremy L Thompson 312ccaff030SJeremy L Thompson *E = rho (c<sub>v</sub> theta Pi + (u u)/2 + g z)* 313ccaff030SJeremy L Thompson 314ccaff030SJeremy L ThompsonConstants: 315ccaff030SJeremy L Thompson 316ccaff030SJeremy L Thompson *theta0* , Potential temperature constant 317ccaff030SJeremy L Thompson 318ccaff030SJeremy L Thompson *thetaC* , Potential temperature perturbation 319ccaff030SJeremy L Thompson 320ccaff030SJeremy L Thompson *P0* , Pressure at the surface 321ccaff030SJeremy L Thompson 322ccaff030SJeremy L Thompson *N* , Brunt-Vaisala frequency 323ccaff030SJeremy L Thompson 324ccaff030SJeremy L Thompson *c<sub>v</sub>* , Specific heat, constant volume 325ccaff030SJeremy L Thompson 326ccaff030SJeremy L Thompson *c<sub>p</sub>* , Specific heat, constant pressure 327ccaff030SJeremy L Thompson 328ccaff030SJeremy L Thompson *R<sub>d</sub>* = c<sub>p</sub> - c<sub>v</sub>, Specific heat difference 329ccaff030SJeremy L Thompson 330ccaff030SJeremy L Thompson *g* , Gravity 331ccaff030SJeremy L Thompson 332ccaff030SJeremy L Thompson *r<sub>c</sub>* , Characteristic radius of thermal bubble 333ccaff030SJeremy L Thompson 334ccaff030SJeremy L Thompson *l<sub>x</sub>* , Characteristic length scale of domain in x 335ccaff030SJeremy L Thompson 336ccaff030SJeremy L Thompson *l<sub>y</sub>* , Characteristic length scale of domain in y 337ccaff030SJeremy L Thompson 338ccaff030SJeremy L Thompson *l<sub>z</sub>* , Characteristic length scale of domain in z 339ccaff030SJeremy L Thompson 340ccaff030SJeremy L Thompson 341ccaff030SJeremy L Thompson#### Boundary Conditions 342ccaff030SJeremy L Thompson 343ccaff030SJeremy L ThompsonMass Density: 344ccaff030SJeremy L Thompson 0.0 flux 345ccaff030SJeremy L Thompson 346ccaff030SJeremy L ThompsonMomentum Density: 347ccaff030SJeremy L Thompson 0.0 348ccaff030SJeremy L Thompson 349ccaff030SJeremy L ThompsonEnergy Density: 350ccaff030SJeremy L Thompson 0.0 flux 351ccaff030SJeremy L Thompson 352ccaff030SJeremy L Thompson### Time Discretization 353ccaff030SJeremy L Thompson 354c063f476SvaleriabarraFor all different problems, the time integration is performed with an explicit 355c063f476Svaleriabarraor implicit formulation. 356ccaff030SJeremy L Thompson 357ccaff030SJeremy L Thompson### Space Discretization 358ccaff030SJeremy L Thompson 359ccaff030SJeremy L ThompsonThe geometric factors and coordinate transformations required for the integration of the weak form 360*89d0f5c0SLeila Ghaffarifor the interior domain and for the boundaries are described in the files [`common.h`](common.h) 361*89d0f5c0SLeila Ghaffariand [`setup-boundary.h`](setup-boundary.h), respectively. 362