1*ea10196cSJeremy L Thompson## libCEED: Navier-Stokes Example 2*ea10196cSJeremy L Thompson 3*ea10196cSJeremy L ThompsonThis page provides a description of the Navier-Stokes example for the libCEED library, based on PETSc. 4*ea10196cSJeremy L Thompson 5*ea10196cSJeremy L ThompsonThe Navier-Stokes problem solves the compressible Navier-Stokes equations in three dimensions using an 6*ea10196cSJeremy L Thompsonexplicit time integration. The state variables are mass density, momentum density, and energy density. 7*ea10196cSJeremy L Thompson 8*ea10196cSJeremy L ThompsonThe main Navier-Stokes solver for libCEED is defined in [`navierstokes.c`](navierstokes.c) 9*ea10196cSJeremy L Thompsonwith different problem definitions according to the application of interest. 10*ea10196cSJeremy L Thompson 11*ea10196cSJeremy L ThompsonBuild by using 12*ea10196cSJeremy L Thompson 13*ea10196cSJeremy L Thompson`make` 14*ea10196cSJeremy L Thompson 15*ea10196cSJeremy L Thompsonand run with 16*ea10196cSJeremy L Thompson 17*ea10196cSJeremy L Thompson`./navierstokes -petscspace_degree 1` 18*ea10196cSJeremy L Thompson 19*ea10196cSJeremy L ThompsonAvailable runtime options are: 20*ea10196cSJeremy L Thompson 21*ea10196cSJeremy L Thompson| Option | Meaning | 22*ea10196cSJeremy L Thompson| :----------------------- | :-----------------------------------------------------------------------------------------------| 23*ea10196cSJeremy L Thompson| `-ceed` | CEED resource specifier | 24*ea10196cSJeremy L Thompson| `-test` | Run in test mode | 25*ea10196cSJeremy L Thompson| `-problem` | Problem to solve (`advection`, `advection2d`, or `density_current`) | 26*ea10196cSJeremy L Thompson| `-stab` | Stabilization method | 27*ea10196cSJeremy L Thompson| `-implicit` | Use implicit time integartor formulation | 28*ea10196cSJeremy L Thompson| `-bc_wall` | Use wall boundary conditions on this list of faces | 29*ea10196cSJeremy L Thompson| `-bc_slip_x` | Use slip boundary conditions, for the x component, on this list of faces | 30*ea10196cSJeremy L Thompson| `-bc_slip_y` | Use slip boundary conditions, for the y component, on this list of faces | 31*ea10196cSJeremy L Thompson| `-bc_slip_z` | Use slip boundary conditions, for the z component, on this list of faces | 32*ea10196cSJeremy L Thompson| `-viz_refine` | Use regular refinement for visualization | 33*ea10196cSJeremy L Thompson| `-petscspace_degree` | Polynomial degree of tensor product basis (needs to be set > 0) | 34*ea10196cSJeremy L Thompson| `-units_meter` | 1 meter in scaled length units | 35*ea10196cSJeremy L Thompson| `-units_second` | 1 second in scaled time units | 36*ea10196cSJeremy L Thompson| `-units_kilogram` | 1 kilogram in scaled mass units | 37*ea10196cSJeremy L Thompson| `-units_Kelvin` | 1 Kelvin in scaled temperature units | 38*ea10196cSJeremy L Thompson| `-theta0` | Reference potential temperature | 39*ea10196cSJeremy L Thompson| `-thetaC` | Perturbation of potential temperature | 40*ea10196cSJeremy L Thompson| `-P0` | Atmospheric pressure | 41*ea10196cSJeremy L Thompson| `-N` | Brunt-Vaisala frequency | 42*ea10196cSJeremy L Thompson| `-cv` | Heat capacity at constant volume | 43*ea10196cSJeremy L Thompson| `-cp` | Heat capacity at constant pressure | 44*ea10196cSJeremy L Thompson| `-g` | Gravitational acceleration | 45*ea10196cSJeremy L Thompson| `-lambda` | Stokes hypothesis second viscosity coefficient | 46*ea10196cSJeremy L Thompson| `-mu` | Shear dynamic viscosity coefficient | 47*ea10196cSJeremy L Thompson| `-k` | Thermal conductivity | 48*ea10196cSJeremy L Thompson| `-CtauS` | Scale coefficient for stabilization tau (nondimensional) | 49*ea10196cSJeremy L Thompson| `-strong_form` | Strong (1) or weak/integrated by parts (0) advection residual | 50*ea10196cSJeremy L Thompson| `-lx` | Length scale in x direction | 51*ea10196cSJeremy L Thompson| `-ly` | Length scale in y direction | 52*ea10196cSJeremy L Thompson| `-lz` | Length scale in z direction | 53*ea10196cSJeremy L Thompson| `-rc` | Characteristic radius of thermal bubble | 54*ea10196cSJeremy L Thompson| `-resx` | Resolution in x | 55*ea10196cSJeremy L Thompson| `-resy` | Resolution in y | 56*ea10196cSJeremy L Thompson| `-resz` | Resolution in z | 57*ea10196cSJeremy L Thompson| `-periodicity` | Periodicity per direction | 58*ea10196cSJeremy L Thompson| `-center` | Location of bubble center | 59*ea10196cSJeremy L Thompson| `-dc_axis` | Axis of density current cylindrical anomaly, or {0,0,0} for spherically symmetric | 60*ea10196cSJeremy L Thompson| `-output_freq` | Frequency of output, in number of steps | 61*ea10196cSJeremy L Thompson| `-continue` | Continue from previous solution | 62*ea10196cSJeremy L Thompson| `-degree` | Polynomial degree of tensor product basis | 63*ea10196cSJeremy L Thompson| `-qextra` | Number of extra quadrature points | 64*ea10196cSJeremy L Thompson| `-of` | Output folder | 65*ea10196cSJeremy L Thompson 66*ea10196cSJeremy L Thompson 67*ea10196cSJeremy L Thompson### Advection 68*ea10196cSJeremy L Thompson 69*ea10196cSJeremy L ThompsonThis problem solves the convection (advection) equation for the total (scalar) energy density, 70*ea10196cSJeremy L Thompsontransported by the (vector) velocity field. 71*ea10196cSJeremy L Thompson 72*ea10196cSJeremy L ThompsonThis is 3D advection given in two formulations based upon the weak form. 73*ea10196cSJeremy L Thompson 74*ea10196cSJeremy L ThompsonState Variables: 75*ea10196cSJeremy L Thompson 76*ea10196cSJeremy L Thompson *q = ( rho, U<sub>1</sub>, U<sub>2</sub>, U<sub>3</sub>, E )* 77*ea10196cSJeremy L Thompson 78*ea10196cSJeremy L Thompson *rho* - Mass Density 79*ea10196cSJeremy L Thompson 80*ea10196cSJeremy L Thompson *U<sub>i</sub>* - Momentum Density , *U<sub>i</sub> = rho ui* 81*ea10196cSJeremy L Thompson 82*ea10196cSJeremy L Thompson *E* - Total Energy Density, *E = rho Cv T + rho (u u) / 2 + rho g z* 83*ea10196cSJeremy L Thompson 84*ea10196cSJeremy L ThompsonAdvection Equation: 85*ea10196cSJeremy L Thompson 86*ea10196cSJeremy L Thompson *dE/dt + div( E _u_ ) = 0* 87*ea10196cSJeremy L Thompson 88*ea10196cSJeremy L Thompson#### Initial Conditions 89*ea10196cSJeremy L Thompson 90*ea10196cSJeremy L ThompsonMass Density: 91*ea10196cSJeremy L Thompson Constant mass density of 1.0 92*ea10196cSJeremy L Thompson 93*ea10196cSJeremy L ThompsonMomentum Density: 94*ea10196cSJeremy L Thompson Rotational field in x,y with no momentum in z 95*ea10196cSJeremy L Thompson 96*ea10196cSJeremy L ThompsonEnergy Density: 97*ea10196cSJeremy L Thompson Maximum of 1. x0 decreasing linearly to 0. as radial distance increases 98*ea10196cSJeremy L Thompson to 1/8, then 0. everywhere else 99*ea10196cSJeremy L Thompson 100*ea10196cSJeremy L Thompson#### Boundary Conditions 101*ea10196cSJeremy L Thompson 102*ea10196cSJeremy L ThompsonMass Density: 103*ea10196cSJeremy L Thompson 0.0 flux 104*ea10196cSJeremy L Thompson 105*ea10196cSJeremy L ThompsonMomentum Density: 106*ea10196cSJeremy L Thompson 0.0 107*ea10196cSJeremy L Thompson 108*ea10196cSJeremy L ThompsonEnergy Density: 109*ea10196cSJeremy L Thompson 0.0 flux 110*ea10196cSJeremy L Thompson 111*ea10196cSJeremy L Thompson### Density Current 112*ea10196cSJeremy L Thompson 113*ea10196cSJeremy L ThompsonThis problem solves the full compressible Navier-Stokes equations, using 114*ea10196cSJeremy L Thompsonoperator composition and design of coupled solvers in the context of atmospheric 115*ea10196cSJeremy L Thompsonmodeling. This problem uses the formulation given in Semi-Implicit Formulations 116*ea10196cSJeremy L Thompsonof the Navier-Stokes Equations: Application to Nonhydrostatic Atmospheric Modeling, 117*ea10196cSJeremy L ThompsonGiraldo, Restelli, and Lauter (2010). 118*ea10196cSJeremy L Thompson 119*ea10196cSJeremy L ThompsonThe 3D compressible Navier-Stokes equations are formulated in conservation form with state 120*ea10196cSJeremy L Thompsonvariables of density, momentum density, and total energy density. 121*ea10196cSJeremy L Thompson 122*ea10196cSJeremy L ThompsonState Variables: 123*ea10196cSJeremy L Thompson 124*ea10196cSJeremy L Thompson *q = ( rho, U<sub>1</sub>, U<sub>2</sub>, U<sub>3</sub>, E )* 125*ea10196cSJeremy L Thompson 126*ea10196cSJeremy L Thompson *rho* - Mass Density 127*ea10196cSJeremy L Thompson 128*ea10196cSJeremy L Thompson *U<sub>i</sub>* - Momentum Density , *U<sub>i</sub> = rho u<sub>i</sub>* 129*ea10196cSJeremy L Thompson 130*ea10196cSJeremy L Thompson *E* - Total Energy Density, *E = rho c<sub>v</sub> T + rho (u u) / 2 + rho g z* 131*ea10196cSJeremy L Thompson 132*ea10196cSJeremy L ThompsonNavier-Stokes Equations: 133*ea10196cSJeremy L Thompson 134*ea10196cSJeremy L Thompson *drho/dt + div( U ) = 0* 135*ea10196cSJeremy L Thompson 136*ea10196cSJeremy L Thompson *dU/dt + div( rho (u x u) + P I<sub>3</sub> ) + rho g khat = div( F<sub>u</sub> )* 137*ea10196cSJeremy L Thompson 138*ea10196cSJeremy L Thompson *dE/dt + div( (E + P) u ) = div( F<sub>e</sub> )* 139*ea10196cSJeremy L Thompson 140*ea10196cSJeremy L ThompsonViscous Stress: 141*ea10196cSJeremy L Thompson 142*ea10196cSJeremy L Thompson *F<sub>u</sub> = mu (grad( u ) + grad( u )^T + lambda div ( u ) I<sub>3</sub>)* 143*ea10196cSJeremy L Thompson 144*ea10196cSJeremy L ThompsonThermal Stress: 145*ea10196cSJeremy L Thompson 146*ea10196cSJeremy L Thompson *F<sub>e</sub> = u F<sub>u</sub> + k grad( T )* 147*ea10196cSJeremy L Thompson 148*ea10196cSJeremy L ThompsonEquation of State: 149*ea10196cSJeremy L Thompson 150*ea10196cSJeremy L Thompson *P = (gamma - 1) (E - rho (u u) / 2 - rho g z)* 151*ea10196cSJeremy L Thompson 152*ea10196cSJeremy L ThompsonTemperature: 153*ea10196cSJeremy L Thompson 154*ea10196cSJeremy L Thompson *T = (E / rho - (u u) / 2 - g z) / c<sub>v</sub>* 155*ea10196cSJeremy L Thompson 156*ea10196cSJeremy L ThompsonConstants: 157*ea10196cSJeremy L Thompson 158*ea10196cSJeremy L Thompson *lambda = - 2 / 3*, From Stokes hypothesis 159*ea10196cSJeremy L Thompson 160*ea10196cSJeremy L Thompson *mu* , Dynamic viscosity 161*ea10196cSJeremy L Thompson 162*ea10196cSJeremy L Thompson *k* , Thermal conductivity 163*ea10196cSJeremy L Thompson 164*ea10196cSJeremy L Thompson *c<sub>v</sub>* , Specific heat, constant volume 165*ea10196cSJeremy L Thompson 166*ea10196cSJeremy L Thompson *c<sub>p</sub>* , Specific heat, constant pressure 167*ea10196cSJeremy L Thompson 168*ea10196cSJeremy L Thompson *g* , Gravity 169*ea10196cSJeremy L Thompson 170*ea10196cSJeremy L Thompson *gamma = c<sub>p</sub> / c<sub>v</sub>*, Specific heat ratio 171*ea10196cSJeremy L Thompson 172*ea10196cSJeremy L Thompson#### Initial Conditions 173*ea10196cSJeremy L Thompson 174*ea10196cSJeremy L ThompsonPotential Temperature: 175*ea10196cSJeremy L Thompson 176*ea10196cSJeremy L Thompson *theta = thetabar + deltatheta* 177*ea10196cSJeremy L Thompson 178*ea10196cSJeremy L Thompson *thetabar = theta0 exp( N * * 2 z / g )* 179*ea10196cSJeremy L Thompson 180*ea10196cSJeremy L Thompson *deltatheta = 181*ea10196cSJeremy L Thompson r <= rc : theta0(1 + cos(pi r)) / 2 182*ea10196cSJeremy L Thompson r > rc : 0* 183*ea10196cSJeremy L Thompson 184*ea10196cSJeremy L Thompson *r = sqrt( (x - xc) * * 2 + (y - yc) * * 2 + (z - zc) * * 2 )* 185*ea10196cSJeremy L Thompson with *(xc,yc,zc)* center of domain 186*ea10196cSJeremy L Thompson 187*ea10196cSJeremy L ThompsonExner Pressure: 188*ea10196cSJeremy L Thompson 189*ea10196cSJeremy L Thompson *Pi = Pibar + deltaPi* 190*ea10196cSJeremy L Thompson 191*ea10196cSJeremy L Thompson *Pibar = g * * 2 (exp( - N * * 2 z / g ) - 1) / (cp theta0 N * * 2)* 192*ea10196cSJeremy L Thompson 193*ea10196cSJeremy L Thompson *deltaPi = 0* (hydrostatic balance) 194*ea10196cSJeremy L Thompson 195*ea10196cSJeremy L ThompsonVelocity/Momentum Density: 196*ea10196cSJeremy L Thompson 197*ea10196cSJeremy L Thompson *U<sub>i</sub> = u<sub>i</sub> = 0* 198*ea10196cSJeremy L Thompson 199*ea10196cSJeremy L ThompsonConversion to Conserved Variables: 200*ea10196cSJeremy L Thompson 201*ea10196cSJeremy L Thompson *rho = P0 Pi**(c<sub>v</sub>/R<sub>d</sub>) / (R<sub>d</sub> theta)* 202*ea10196cSJeremy L Thompson 203*ea10196cSJeremy L Thompson *E = rho (c<sub>v</sub> theta Pi + (u u)/2 + g z)* 204*ea10196cSJeremy L Thompson 205*ea10196cSJeremy L ThompsonConstants: 206*ea10196cSJeremy L Thompson 207*ea10196cSJeremy L Thompson *theta0* , Potential temperature constant 208*ea10196cSJeremy L Thompson 209*ea10196cSJeremy L Thompson *thetaC* , Potential temperature perturbation 210*ea10196cSJeremy L Thompson 211*ea10196cSJeremy L Thompson *P0* , Pressure at the surface 212*ea10196cSJeremy L Thompson 213*ea10196cSJeremy L Thompson *N* , Brunt-Vaisala frequency 214*ea10196cSJeremy L Thompson 215*ea10196cSJeremy L Thompson *c<sub>v</sub>* , Specific heat, constant volume 216*ea10196cSJeremy L Thompson 217*ea10196cSJeremy L Thompson *c<sub>p</sub>* , Specific heat, constant pressure 218*ea10196cSJeremy L Thompson 219*ea10196cSJeremy L Thompson *R<sub>d</sub>* = c<sub>p</sub> - c<sub>v</sub>, Specific heat difference 220*ea10196cSJeremy L Thompson 221*ea10196cSJeremy L Thompson *g* , Gravity 222*ea10196cSJeremy L Thompson 223*ea10196cSJeremy L Thompson *r<sub>c</sub>* , Characteristic radius of thermal bubble 224*ea10196cSJeremy L Thompson 225*ea10196cSJeremy L Thompson *l<sub>x</sub>* , Characteristic length scale of domain in x 226*ea10196cSJeremy L Thompson 227*ea10196cSJeremy L Thompson *l<sub>y</sub>* , Characteristic length scale of domain in y 228*ea10196cSJeremy L Thompson 229*ea10196cSJeremy L Thompson *l<sub>z</sub>* , Characteristic length scale of domain in z 230*ea10196cSJeremy L Thompson 231*ea10196cSJeremy L Thompson 232*ea10196cSJeremy L Thompson#### Boundary Conditions 233*ea10196cSJeremy L Thompson 234*ea10196cSJeremy L ThompsonMass Density: 235*ea10196cSJeremy L Thompson 0.0 flux 236*ea10196cSJeremy L Thompson 237*ea10196cSJeremy L ThompsonMomentum Density: 238*ea10196cSJeremy L Thompson 0.0 239*ea10196cSJeremy L Thompson 240*ea10196cSJeremy L ThompsonEnergy Density: 241*ea10196cSJeremy L Thompson 0.0 flux 242*ea10196cSJeremy L Thompson 243*ea10196cSJeremy L Thompson### Time Discretization 244*ea10196cSJeremy L Thompson 245*ea10196cSJeremy L ThompsonFor all different problems, the time integration is performed with an explicit formulation, therefore 246*ea10196cSJeremy L Thompsonit can be subject to numerical instability, if run for large times or with large time steps. 247*ea10196cSJeremy L Thompson 248*ea10196cSJeremy L Thompson### Space Discretization 249*ea10196cSJeremy L Thompson 250*ea10196cSJeremy L ThompsonThe geometric factors and coordinate transformations required for the integration of the weak form 251*ea10196cSJeremy L Thompsonare described in the file [`common.h`](common.h) 252