Source code for pyro.lm_atm.simulation

import importlib

import matplotlib.pyplot as plt
import numpy as np

import pyro.lm_atm.LM_atm_interface as lm_interface
import pyro.mesh.array_indexer as ai
import pyro.mesh.boundary as bnd
import pyro.multigrid.variable_coeff_MG as vcMG
from pyro.mesh import patch, reconstruction
from pyro.simulation_null import NullSimulation, bc_setup, grid_setup


[docs] class Basestate: def __init__(self, ny, ng=0): self.ny = ny self.ng = ng self.qy = ny + 2*ng self.d = np.zeros((self.qy), dtype=np.float64) self.jlo = ng self.jhi = ng+ny-1
[docs] def v(self, buf=0): return self.d[self.jlo-buf:self.jhi+1+buf]
[docs] def v2d(self, buf=0): return self.d[np.newaxis, self.jlo-buf:self.jhi+1+buf]
[docs] def v2dp(self, shift, buf=0): return self.d[np.newaxis, self.jlo+shift-buf:self.jhi+1+shift+buf]
[docs] def jp(self, shift, buf=0): return self.d[self.jlo-buf+shift:self.jhi+1+buf+shift]
[docs] class Simulation(NullSimulation): def __init__(self, solver_name, problem_name, rp, timers=None): NullSimulation.__init__(self, solver_name, problem_name, rp, timers=timers) self.base = {} self.aux_data = None self.in_preevolve = False
[docs] def initialize(self): """ Initialize the grid and variables for low Mach atmospheric flow and set the initial conditions for the chosen problem. """ myg = grid_setup(self.rp, ng=4) bc_dens, bc_xodd, bc_yodd = bc_setup(self.rp) my_data = patch.CellCenterData2d(myg) my_data.register_var("density", bc_dens) my_data.register_var("x-velocity", bc_xodd) my_data.register_var("y-velocity", bc_yodd) # we'll keep the internal energy around just as a diagnostic my_data.register_var("eint", bc_dens) # phi -- used for the projections. The boundary conditions # here depend on velocity. At a wall or inflow, we already # have the velocity we want on the boundary, so we want # Neumann (dphi/dn = 0). For outflow, we want Dirichlet (phi # = 0) -- this ensures that we do not introduce any tangental # acceleration. bcs = [] for bc in [self.rp.get_param("mesh.xlboundary"), self.rp.get_param("mesh.xrboundary"), self.rp.get_param("mesh.ylboundary"), self.rp.get_param("mesh.yrboundary")]: if bc == "periodic": bctype = "periodic" elif bc in ["reflect", "slipwall"]: bctype = "neumann" elif bc in ["outflow"]: bctype = "dirichlet" bcs.append(bctype) bc_phi = bnd.BC(xlb=bcs[0], xrb=bcs[1], ylb=bcs[2], yrb=bcs[3]) my_data.register_var("phi-MAC", bc_phi) my_data.register_var("phi", bc_phi) # gradp -- used in the projection and interface states. We'll do the # same BCs as density my_data.register_var("gradp_x", bc_dens) my_data.register_var("gradp_y", bc_dens) my_data.create() self.cc_data = my_data # some auxiliary data that we'll need to fill GC in, but isn't # really part of the main solution aux_data = patch.CellCenterData2d(myg) aux_data.register_var("coeff", bc_dens) aux_data.register_var("source_y", bc_yodd) aux_data.create() self.aux_data = aux_data # we also need storage for the 1-d base state -- we'll store this # in the main class directly. self.base["rho0"] = Basestate(myg.ny, ng=myg.ng) self.base["p0"] = Basestate(myg.ny, ng=myg.ng) # now set the initial conditions for the problem problem = importlib.import_module(f"pyro.lm_atm.problems.{self.problem_name}") problem.init_data(self.cc_data, self.base, self.rp) # Construct beta_0 gamma = self.rp.get_param("eos.gamma") self.base["beta0"] = Basestate(myg.ny, ng=myg.ng) self.base["beta0"].d[:] = self.base["p0"].d**(1.0/gamma) # we'll also need beta_0 on vertical edges -- on the domain edges, # just do piecewise constant self.base["beta0-edges"] = Basestate(myg.ny, ng=myg.ng) self.base["beta0-edges"].jp(1)[:] = \ 0.5*(self.base["beta0"].v() + self.base["beta0"].jp(1)) self.base["beta0-edges"].d[myg.jlo] = self.base["beta0"].d[myg.jlo] self.base["beta0-edges"].d[myg.jhi+1] = self.base["beta0"].d[myg.jhi]
[docs] def make_prime(self, a, a0): return a - a0.v2d(buf=a0.ng)
[docs] def method_compute_timestep(self): """ The timestep() function computes the advective timestep (CFL) constraint. The CFL constraint says that information cannot propagate further than one zone per timestep. We use the driver.cfl parameter to control what fraction of the CFL step we actually take. """ myg = self.cc_data.grid cfl = self.rp.get_param("driver.cfl") u = self.cc_data.get_var("x-velocity") v = self.cc_data.get_var("y-velocity") # the timestep is min(dx/|u|, dy|v|) xtmp = ytmp = 1.e33 if not abs(u).max() == 0: xtmp = myg.dx/abs(u.v()).max() if not abs(v).max() == 0: ytmp = myg.dy/abs(v.v()).max() dt = cfl*min(xtmp, ytmp) # We need an alternate timestep that accounts for buoyancy, to # handle the case where the velocity is initially zero. rho = self.cc_data.get_var("density") rho0 = self.base["rho0"] rhoprime = self.make_prime(rho, rho0) g = self.rp.get_param("lm-atmosphere.grav") F_buoy = (abs(rhoprime*g).v()/rho.v()).max() dt_buoy = np.sqrt(2.0*myg.dx/F_buoy) self.dt = min(dt, dt_buoy) if self.verbose > 0: print(f"timestep is {dt}")
[docs] def preevolve(self): """ preevolve is called before we being the timestepping loop. For the low Mach solver, this does an initial projection on the velocity field and then goes through the full evolution to get the value of phi. The fluid state (rho, u, v) is then reset to values before this evolve. """ self.in_preevolve = True myg = self.cc_data.grid rho = self.cc_data.get_var("density") u = self.cc_data.get_var("x-velocity") v = self.cc_data.get_var("y-velocity") self.cc_data.fill_BC("density") self.cc_data.fill_BC("x-velocity") self.cc_data.fill_BC("y-velocity") # 1. do the initial projection. This makes sure that our original # velocity field satisties div U = 0 # the coefficient for the elliptic equation is beta_0^2/rho coeff = 1/rho beta0 = self.base["beta0"] coeff.v()[:, :] = coeff.v()*beta0.v2d()**2 # next create the multigrid object. We defined phi with # the right BCs previously mg = vcMG.VarCoeffCCMG2d(myg.nx, myg.ny, xl_BC_type=self.cc_data.BCs["phi"].xlb, xr_BC_type=self.cc_data.BCs["phi"].xrb, yl_BC_type=self.cc_data.BCs["phi"].ylb, yr_BC_type=self.cc_data.BCs["phi"].yrb, xmin=myg.xmin, xmax=myg.xmax, ymin=myg.ymin, ymax=myg.ymax, coeffs=coeff, coeffs_bc=self.cc_data.BCs["density"], verbose=0) # first compute div{beta_0 U} div_beta_U = mg.soln_grid.scratch_array() # u/v are cell-centered, divU is cell-centered div_beta_U.v()[:, :] = \ 0.5*beta0.v2d()*(u.ip(1) - u.ip(-1))/myg.dx + \ 0.5*(beta0.v2dp(1)*v.jp(1) - beta0.v2dp(-1)*v.jp(-1))/myg.dy # solve D (beta_0^2/rho) G (phi/beta_0) = D( beta_0 U ) # set the RHS to divU and solve mg.init_RHS(div_beta_U) mg.solve(rtol=1.e-10) # store the solution in our self.cc_data object -- include a single # ghostcell phi = self.cc_data.get_var("phi") phi[:, :] = mg.get_solution(grid=myg) # get the cell-centered gradient of phi and update the # velocities # FIXME: this update only needs to be done on the interior # cells -- not ghost cells gradp_x, gradp_y = mg.get_solution_gradient(grid=myg) coeff = 1.0/rho coeff.v()[:, :] = coeff.v()*beta0.v2d() u.v()[:, :] -= coeff.v()*gradp_x.v() v.v()[:, :] -= coeff.v()*gradp_y.v() # fill the ghostcells self.cc_data.fill_BC("x-velocity") self.cc_data.fill_BC("y-velocity") # 2. now get an approximation to gradp at n-1/2 by going through the # evolution. # store the current solution -- we'll restore it in a bit orig_data = patch.cell_center_data_clone(self.cc_data) # get the timestep self.method_compute_timestep() # evolve self.evolve() # update gradp_x and gradp_y in our main data object new_gp_x = self.cc_data.get_var("gradp_x") new_gp_y = self.cc_data.get_var("gradp_y") orig_gp_x = orig_data.get_var("gradp_x") orig_gp_y = orig_data.get_var("gradp_y") orig_gp_x[:, :] = new_gp_x[:, :] orig_gp_y[:, :] = new_gp_y[:, :] self.cc_data = orig_data if self.verbose > 0: print("done with the pre-evolution") self.in_preevolve = False
[docs] def evolve(self): """ Evolve the low Mach system through one timestep. """ rho = self.cc_data.get_var("density") u = self.cc_data.get_var("x-velocity") v = self.cc_data.get_var("y-velocity") gradp_x = self.cc_data.get_var("gradp_x") gradp_y = self.cc_data.get_var("gradp_y") # note: the base state quantities do not have valid ghost cells beta0 = self.base["beta0"] beta0_edges = self.base["beta0-edges"] rho0 = self.base["rho0"] phi = self.cc_data.get_var("phi") myg = self.cc_data.grid # --------------------------------------------------------------------- # create the limited slopes of rho, u and v (in both directions) # --------------------------------------------------------------------- limiter = self.rp.get_param("lm-atmosphere.limiter") ldelta_rx = reconstruction.limit(rho, myg, 1, limiter) ldelta_ux = reconstruction.limit(u, myg, 1, limiter) ldelta_vx = reconstruction.limit(v, myg, 1, limiter) ldelta_ry = reconstruction.limit(rho, myg, 2, limiter) ldelta_uy = reconstruction.limit(u, myg, 2, limiter) ldelta_vy = reconstruction.limit(v, myg, 2, limiter) # --------------------------------------------------------------------- # get the advective velocities # --------------------------------------------------------------------- """ the advective velocities are the normal velocity through each cell interface, and are defined on the cell edges, in a MAC type staggered form n+1/2 v i,j+1/2 +------+------+ | | n+1/2 | | n+1/2 u + U + u i-1/2,j | i,j | i+1/2,j | | +------+------+ n+1/2 v i,j-1/2 """ # this returns u on x-interfaces and v on y-interfaces. These # constitute the MAC grid if self.verbose > 0: print(" making MAC velocities") # create the coefficient to the grad (pi/beta) term coeff = self.aux_data.get_var("coeff") coeff.v()[:, :] = 1.0/rho.v() coeff.v()[:, :] = coeff.v()*beta0.v2d() self.aux_data.fill_BC("coeff") # create the source term source = self.aux_data.get_var("source_y") g = self.rp.get_param("lm-atmosphere.grav") rhoprime = self.make_prime(rho, rho0) source.v()[:, :] = rhoprime.v()*g/rho.v() self.aux_data.fill_BC("source_y") _um, _vm = lm_interface.mac_vels(myg.ng, myg.dx, myg.dy, self.dt, u, v, ldelta_ux, ldelta_vx, ldelta_uy, ldelta_vy, coeff*gradp_x, coeff*gradp_y, source) u_MAC = ai.ArrayIndexer(d=_um, grid=myg) v_MAC = ai.ArrayIndexer(d=_vm, grid=myg) # --------------------------------------------------------------------- # do a MAC projection to make the advective velocities divergence # free # --------------------------------------------------------------------- # we will solve D (beta_0^2/rho) G phi = D (beta_0 U^MAC), where # phi is cell centered, and U^MAC is the MAC-type staggered # grid of the advective velocities. if self.verbose > 0: print(" MAC projection") # create the coefficient array: beta0**2/rho # MZ!!!! probably don't need the buf here coeff.v(buf=1)[:, :] = 1.0/rho.v(buf=1) coeff.v(buf=1)[:, :] = coeff.v(buf=1)*beta0.v2d(buf=1)**2 # create the multigrid object mg = vcMG.VarCoeffCCMG2d(myg.nx, myg.ny, xl_BC_type=self.cc_data.BCs["phi-MAC"].xlb, xr_BC_type=self.cc_data.BCs["phi-MAC"].xrb, yl_BC_type=self.cc_data.BCs["phi-MAC"].ylb, yr_BC_type=self.cc_data.BCs["phi-MAC"].yrb, xmin=myg.xmin, xmax=myg.xmax, ymin=myg.ymin, ymax=myg.ymax, coeffs=coeff, coeffs_bc=self.cc_data.BCs["density"], verbose=0) # first compute div{beta_0 U} div_beta_U = mg.soln_grid.scratch_array() # MAC velocities are edge-centered. div{beta_0 U} is cell-centered. div_beta_U.v()[:, :] = \ beta0.v2d()*(u_MAC.ip(1) - u_MAC.v())/myg.dx + \ (beta0_edges.v2dp(1)*v_MAC.jp(1) - beta0_edges.v2d()*v_MAC.v())/myg.dy # solve the Poisson problem mg.init_RHS(div_beta_U) mg.solve(rtol=1.e-12) # update the normal velocities with the pressure gradient -- these # constitute our advective velocities. Note that what we actually # solved for here is phi/beta_0 phi_MAC = self.cc_data.get_var("phi-MAC") phi_MAC[:, :] = mg.get_solution(grid=myg) coeff = self.aux_data.get_var("coeff") coeff.v()[:, :] = 1.0/rho.v() coeff.v()[:, :] = coeff.v()*beta0.v2d() self.aux_data.fill_BC("coeff") coeff_x = myg.scratch_array() b = (3, 1, 0, 0) # this seems more than we need coeff_x.v(buf=b)[:, :] = 0.5*(coeff.ip(-1, buf=b) + coeff.v(buf=b)) coeff_y = myg.scratch_array() b = (0, 0, 3, 1) coeff_y.v(buf=b)[:, :] = 0.5*(coeff.jp(-1, buf=b) + coeff.v(buf=b)) # we need the MAC velocities on all edges of the computational domain # here we do U = U - (beta_0/rho) grad (phi/beta_0) b = (0, 1, 0, 0) u_MAC.v(buf=b)[:, :] -= \ coeff_x.v(buf=b)*(phi_MAC.v(buf=b) - phi_MAC.ip(-1, buf=b))/myg.dx b = (0, 0, 0, 1) v_MAC.v(buf=b)[:, :] -= \ coeff_y.v(buf=b)*(phi_MAC.v(buf=b) - phi_MAC.jp(-1, buf=b))/myg.dy # --------------------------------------------------------------------- # predict rho to the edges and do its conservative update # --------------------------------------------------------------------- _rx, _ry = lm_interface.rho_states(myg.ng, myg.dx, myg.dy, self.dt, rho, u_MAC, v_MAC, ldelta_rx, ldelta_ry) rho_xint = ai.ArrayIndexer(d=_rx, grid=myg) rho_yint = ai.ArrayIndexer(d=_ry, grid=myg) rho_old = rho.copy() rho.v()[:, :] -= self.dt*( # (rho u)_x (rho_xint.ip(1)*u_MAC.ip(1) - rho_xint.v()*u_MAC.v())/myg.dx + # (rho v)_y (rho_yint.jp(1)*v_MAC.jp(1) - rho_yint.v()*v_MAC.v())/myg.dy) self.cc_data.fill_BC("density") # update eint as a diagnostic eint = self.cc_data.get_var("eint") gamma = self.rp.get_param("eos.gamma") eint.v()[:, :] = self.base["p0"].v2d()/(gamma - 1.0)/rho.v() # --------------------------------------------------------------------- # recompute the interface states, using the advective velocity # from above # --------------------------------------------------------------------- if self.verbose > 0: print(" making u, v edge states") coeff = self.aux_data.get_var("coeff") coeff.v()[:, :] = 2.0/(rho.v() + rho_old.v()) coeff.v()[:, :] = coeff.v()*beta0.v2d() self.aux_data.fill_BC("coeff") _ux, _vx, _uy, _vy = \ lm_interface.states(myg.ng, myg.dx, myg.dy, self.dt, u, v, ldelta_ux, ldelta_vx, ldelta_uy, ldelta_vy, coeff*gradp_x, coeff*gradp_y, source, u_MAC, v_MAC) u_xint = ai.ArrayIndexer(d=_ux, grid=myg) v_xint = ai.ArrayIndexer(d=_vx, grid=myg) u_yint = ai.ArrayIndexer(d=_uy, grid=myg) v_yint = ai.ArrayIndexer(d=_vy, grid=myg) # --------------------------------------------------------------------- # update U to get the provisional velocity field # --------------------------------------------------------------------- if self.verbose > 0: print(" doing provisional update of u, v") # compute (U.grad)U # we want u_MAC U_x + v_MAC U_y advect_x = myg.scratch_array() advect_y = myg.scratch_array() advect_x.v()[:, :] = \ 0.5*(u_MAC.v() + u_MAC.ip(1))*(u_xint.ip(1) - u_xint.v())/myg.dx +\ 0.5*(v_MAC.v() + v_MAC.jp(1))*(u_yint.jp(1) - u_yint.v())/myg.dy advect_y.v()[:, :] = \ 0.5*(u_MAC.v() + u_MAC.ip(1))*(v_xint.ip(1) - v_xint.v())/myg.dx +\ 0.5*(v_MAC.v() + v_MAC.jp(1))*(v_yint.jp(1) - v_yint.v())/myg.dy proj_type = self.rp.get_param("lm-atmosphere.proj_type") if proj_type == 1: u.v()[:, :] -= (self.dt*advect_x.v() + self.dt*gradp_x.v()) v.v()[:, :] -= (self.dt*advect_y.v() + self.dt*gradp_y.v()) elif proj_type == 2: u.v()[:, :] -= self.dt*advect_x.v() v.v()[:, :] -= self.dt*advect_y.v() # add the gravitational source rho_half = 0.5*(rho + rho_old) rhoprime = self.make_prime(rho_half, rho0) source[:, :] = rhoprime*g/rho_half self.aux_data.fill_BC("source_y") v[:, :] += self.dt*source self.cc_data.fill_BC("x-velocity") self.cc_data.fill_BC("y-velocity") if self.verbose > 0: print("min/max rho = {}, {}".format(self.cc_data.min("density"), self.cc_data.max("density"))) print("min/max u = {}, {}".format(self.cc_data.min("x-velocity"), self.cc_data.max("x-velocity"))) print("min/max v = {}, {}".format(self.cc_data.min("y-velocity"), self.cc_data.max("y-velocity"))) # --------------------------------------------------------------------- # project the final velocity # --------------------------------------------------------------------- # now we solve L phi = D (U* /dt) if self.verbose > 0: print(" final projection") # create the coefficient array: beta0**2/rho coeff = 1.0/rho coeff.v()[:, :] = coeff.v()*beta0.v2d()**2 # create the multigrid object mg = vcMG.VarCoeffCCMG2d(myg.nx, myg.ny, xl_BC_type=self.cc_data.BCs["phi"].xlb, xr_BC_type=self.cc_data.BCs["phi"].xrb, yl_BC_type=self.cc_data.BCs["phi"].ylb, yr_BC_type=self.cc_data.BCs["phi"].yrb, xmin=myg.xmin, xmax=myg.xmax, ymin=myg.ymin, ymax=myg.ymax, coeffs=coeff, coeffs_bc=self.cc_data.BCs["density"], verbose=0) # first compute div{beta_0 U} # u/v are cell-centered, divU is cell-centered div_beta_U.v()[:, :] = \ 0.5*beta0.v2d()*(u.ip(1) - u.ip(-1))/myg.dx + \ 0.5*(beta0.v2dp(1)*v.jp(1) - beta0.v2dp(-1)*v.jp(-1))/myg.dy mg.init_RHS(div_beta_U/self.dt) # use the old phi as our initial guess phiGuess = mg.soln_grid.scratch_array() phiGuess.v(buf=1)[:, :] = phi.v(buf=1) mg.init_solution(phiGuess) # solve mg.solve(rtol=1.e-12) # store the solution in our self.cc_data object -- include a single # ghostcell phi[:, :] = mg.get_solution(grid=myg) # get the cell-centered gradient of p and update the velocities # this differs depending on what we projected. gradphi_x, gradphi_y = mg.get_solution_gradient(grid=myg) # U = U - (beta_0/rho) grad (phi/beta_0) coeff = 1.0/rho coeff.v()[:, :] = coeff.v()*beta0.v2d() u.v()[:, :] -= self.dt*coeff.v()*gradphi_x.v() v.v()[:, :] -= self.dt*coeff.v()*gradphi_y.v() # store gradp for the next step if proj_type == 1: gradp_x.v()[:, :] += gradphi_x.v() gradp_y.v()[:, :] += gradphi_y.v() elif proj_type == 2: gradp_x.v()[:, :] = gradphi_x.v() gradp_y.v()[:, :] = gradphi_y.v() self.cc_data.fill_BC("x-velocity") self.cc_data.fill_BC("y-velocity") self.cc_data.fill_BC("gradp_x") self.cc_data.fill_BC("gradp_y") # increment the time if not self.in_preevolve: self.cc_data.t += self.dt self.n += 1
[docs] def dovis(self): """ Do runtime visualization """ plt.clf() # plt.rc("font", size=10) rho = self.cc_data.get_var("density") rho0 = self.base["rho0"] rhoprime = self.make_prime(rho, rho0) u = self.cc_data.get_var("x-velocity") v = self.cc_data.get_var("y-velocity") myg = self.cc_data.grid magvel = np.sqrt(u**2 + v**2) vort = myg.scratch_array() dv = 0.5*(v.ip(1) - v.ip(-1))/myg.dx du = 0.5*(u.jp(1) - u.jp(-1))/myg.dy vort.v()[:, :] = dv - du _, axes = plt.subplots(nrows=2, ncols=2, num=1) plt.subplots_adjust(hspace=0.25) fields = [rho, magvel, vort, rhoprime] field_names = [r"$\rho$", r"|U|", r"$\nabla \times U$", r"$\rho'$"] for n, f in enumerate(fields): ax = axes.flat[n] img = ax.imshow(np.transpose(f.v()), interpolation="nearest", origin="lower", extent=[myg.xmin, myg.xmax, myg.ymin, myg.ymax], cmap=self.cm) ax.set_xlabel("x") ax.set_ylabel("y") ax.set_title(field_names[n]) plt.colorbar(img, ax=ax) plt.figtext(0.05, 0.0125, f"t = {self.cc_data.t:10.5f}") plt.pause(0.001) plt.draw()
[docs] def write_extras(self, f): """ Output simulation-specific data to the h5py file f """ # we implement our own version to allow us to store the base # state gb = f.create_group("base state") for name, state in self.base.items(): gb.create_dataset(name, data=state.d)
[docs] def read_extras(self, f): """ read in any simulation-specific data from an h5py file object f """ gb = f["base state"] for name in gb: self.base[name] = Basestate(self.cc_data.grid.ny, ng=self.cc_data.grid.ng) self.base[name].d[:] = gb[name]