A python hydrodynamics code for teaching and prototyping
Project description
A simple python-based tutorial on computational methods for hydrodynamics
pyro is a computational hydrodynamics code that presents two-dimensional solvers for advection, compressible hydrodynamics, diffusion, incompressible hydrodynamics, and multigrid, all in a finite-volume framework. The code is mainly written in python and is designed with simplicity in mind. The algorithms are written to encourage experimentation and allow for self-learning of these code methods.
The latest version of pyro is always available at:
https://github.com/python-hydro/pyro2
The project webpage, where you'll find documentation, plots, notes, etc. is here:
https://python-hydro.github.io/pyro2
(Note: there is an outdated page at readthedocs.org that is no longer updated)
Table of Contents
- Getting started
- Core Data Structures
- Solvers
- Working with data
- Understanding the algorithms
- Regression and unit testing
- Acknowledgements
- Getting help
Getting started
-
By default, we assume python 3.9 or later.
-
We require
numpy
,numba
,matplotlib
, andh5py
for running pyro andsetuptools_scm
for the install. -
There are several ways to install pyro. The simplest way is via PyPI/pip:
pip install pyro-hydro
Alternately, you can install directly from source, via
pip install .
you can optionally add the
-e
argument toinstall
if you are planning on developing pyro solvers directly. -
Not all matplotlib backends allow for the interactive plotting as pyro is run. One that does is the TkAgg backend. This can be made the default by creating a file
~/.matplotlib/matplotlibrc
with the content:backend: TkAgg
You can check what backend is your current default in python via:
import matplotlib.pyplot print matplotlib.pyplot.get_backend()
-
If you want to run the unit tests, you need to have
pytest
installed. -
Finally, you can run a quick test of the advection solver:
pyro_sim.py advection smooth inputs.smooth
you should see a graphing window pop up with a smooth pulse advecting diagonally through the periodic domain.
Core Data Structures
The main data structures that describe the grid and the data the lives on the grid are described in a jupyter notebook:
https://github.com/python-hydro/pyro2/blob/main/pyro/mesh/mesh-examples.ipynb
Many of the methods here rely on multigrid. The basic multigrid solver is demonstrated in the juputer notebook:
https://github.com/python-hydro/pyro2/blob/main/pyro/multigrid/multigrid-constant-coefficients.ipynb
Solvers
pyro provides the following solvers (all in 2-d):
-
advection
: a second-order unsplit linear advection solver. This uses characteristic tracing and corner coupling for the prediction of the interface states. This is the basic method to understand hydrodynamics. -
advection_fv4
: a fourth-order accurate finite-volume advection solver that uses RK4 time integration. -
advection_nonuniform
: a solver for advection with a non-uniform velocity field. -
advection_rk
: a second-order unsplit solver for linear advection that uses Runge-Kutta integration instead of characteristic tracing. -
advection_weno
: a method-of-lines WENO solver for linear advection. -
burgers
: a second-order unsplit solver for invsicid Burgers' equation. -
burgers_viscous
: a second-order unsplit solver for viscous Burgers' equation with constant-coefficient diffusion. It uses Crank-Nicolson time-discretized solver for solving diffusion. -
compressible
: a second-order unsplit solver for the Euler equations of compressible hydrodynamics. This uses characteristic tracing and corner coupling for the prediction of the interface states and a 2-shock or HLLC approximate Riemann solver. -
compressible_fv4
: a fourth-order accurate finite-volume compressible hydro solver that uses RK4 time integration. This is built from the method of McCourquodale and Colella (2011). -
compressible_rk
: a second-order unsplit solver for Euler equations that uses Runge-Kutta integration instead of characteristic tracing. -
compressible_sdc
: a fourth-order compressible solver, using spectral-deferred correction (SDC) for the time integration. -
diffusion
: a Crank-Nicolson time-discretized solver for the constant-coefficient diffusion equation. -
incompressible
: a second-order cell-centered approximate projection method for the incompressible equations of hydrodynamics. -
incompressible_viscous
: an extension of the incompressible solver including a diffusion term for viscosity. -
lm_atm
: a solver for the equations of low Mach number hydrodynamics for atmospheric flows. -
lm_combustion
: (in development) a solver for the equations of low Mach number hydrodynamics for smallscale combustion. -
multigrid
: a cell-centered multigrid solver for a constant-coefficient Helmholtz equation, as well as a variable-coefficient Poisson equation (which inherits from the constant-coefficient solver). -
particles
: a solver for Lagrangian tracer particles. -
swe
: a solver for the shallow water equations.
Working with data
In addition to the main pyro program, there are many analysis tools that we describe here. Note: some problems write a report at the end of the simulation specifying the analysis routines that can be used with their data.
-
pyro/util/compare.py
: this takes two simulation output files as input and compares zone-by-zone for exact agreement. This is used as part of the regression testing.usage:
./compare.py file1 file2
-
pyro/plot.py
: this takes the an output file as input and plots the data using the solver's dovis method.usage:
./plot.py file
-
pyro/analysis/
-
dam_compare.py
: this takes an output file from the shallow water dam break problem and plots a slice through the domain together with the analytic solution (calculated in the script).usage:
./dam_compare.py file
-
gauss_diffusion_compare.py
: this is for the diffusion solver's Gaussian diffusion problem. It takes a sequence of output files as arguments, computes the angle-average, and the plots the resulting points over the analytic solution for comparison with the exact result.usage:
./gauss_diffusion_compare.py file*
-
incomp_converge_error.py
: this is for the incompressible solver's converge problem. This takes a single output file as input and compares the velocity field to the analytic solution, reporting the L2 norm of the error.usage:
./incomp_converge_error.py file
-
plotvar.py
: this takes a single output file and a variable name and plots the data for that variable.usage:
./plotvar.py file variable
-
sedov_compare.py
: this takes an output file from the compressible Sedov problem, computes the angle-average profile of the solution and plots it together with the analytic data (read in fromcylindrical-sedov.out
).usage:
./sedov_compare.py file
-
smooth_error.py
: this takes an output file from the advection solver's smooth problem and compares to the analytic solution, outputting the L2 norm of the error.usage:
./smooth_error.py file
-
sod_compare.py
: this takes an output file from the compressible Sod problem and plots a slice through the domain over the analytic solution (read in fromsod-exact.out
).usage:
./sod_compare.py file
-
Understanding the algorithms
There is a set of notes that describe the background and details of the algorithms that pyro implements:
http://open-astrophysics-bookshelf.github.io/numerical_exercises/
The source for these notes is also available on github:
https://github.com/Open-Astrophysics-Bookshelf/numerical_exercises
Regression and unit testing
The pyro/test.py
script will run several of the problems (as well
as some stand-alone multigrid tests) and compare the solution to
stored benchmarks (in each solver's tests/
subdirectory). The
return value of the script is the number of tests that failed.
Unit tests are controlled by pytest and can be run simply via
pytest
Acknowledgements
If you use pyro in a class or workshop, please e-mail us to let us know (we'd like to start listing these on the website).
If pyro was used for a publication, please cite the article found in
the CITATION
file.
Getting help
We use github discussions as a way to ask about the code:
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