# The 2D cylindrical shell benchmarks by Davies et al. *This section was contributed by William Durkin and Wolfgang Bangerth.* All of the benchmarks presented so far take place in a Cartesian domain. Davies et al. describe a benchmark (in a paper that is currently still being written) for a 2D spherical Earth that is nondimensionalized such that {table} :name: tab:davies_et_al | | | |:------------------|:---------------------------------| | $r_{\min}$ = 1.22 | $T \|_{r_{min}} = 1$ | | $r_{\max}$ = 2.22 | $T \|_{r_{max}} = 0$ |  The benchmark is run for a series of approximations (Boussinesq, Extended Boussinesq, Truncated Anelastic Liquid, and Anelastic Liquid), and temperature, velocity, and heat flux calculations are compared with the results of other mantle modeling programs. will output all of these values directly except for the Nusselt number, which we must calculate ourselves from the heat fluxes that can compute. The Nusselt number of the top and bottom surfaces, ${Nu}_T$ and ${Nu}_B$, respectively, are defined by the authors of the benchmarks as {math} :label: eq:davies-NuTop {Nu}_{T} = \frac{\ln(f)}{2{\pi}r_{\max}(1-f)}\int \limits_{0}^{2\pi} \frac{\partial T}{\partial r}\, \text{d}\theta  and {math} :label: eq:davies-NuBottom {Nu}_{B} = \frac{f \ln(f)}{2{\pi}r_{\min}(1-f)}\int \limits_{0}^{2\pi} \frac{\partial T}{\partial r}\, \text{d}\theta  where $f$ is the ratio $\frac{r_{\min}}{r_{\max}}$. We can put this in terms of heat flux {math} q_r = -k\frac{\partial T}{\partial r}  through the inner and outer surfaces, where $q_r$ is heat flux in the radial direction. Let $Q$ be the total heat that flows through a surface, {math} Q = \int \limits_{0}^{2\pi} q_r\, \text{d}\theta,  then {math:numref}eq:davies-NuTop becomes {math} {Nu}_{T} = \frac{-Q_{T}\ln(f)}{2\pi{r_{\max}}(1-f)k}  and similarly {math} {Nu}_{B} = \frac{-Q_{B}f\ln(f)}{2\pi{r_{\min}}(1-f)k}.  $Q_T$ and $Q_B$ are heat fluxes that can readily compute through the heat flux statistics postprocessor (see {ref}parameters:Postprocess/List_20of_20postprocessors). For further details on the nondimensionalization and equations used for each approximation, refer to Davies et al. The series of benchmarks is then defined by a number of cases relating to the exact equations chosen to model the fluid. We will discuss these in the following. ## Case 1.1: BA_Ra104_Iso_ZS. This case is run with the following settings: - Boussinesq Approximation - Boundary Condition: Zero-Slip - Rayleigh Number = $10^4$ - Initial Conditions: $D = 0, O = 4$ - $\eta(T) = 1$ where $D$ and $O$ refer to the degree and order of a spherical harmonic that describes the initial temperature. While the initial conditions matter, what is important here though is that the system evolve to four convective cells since we are only interested in the long term, steady state behavior. The model is relatively straightforward to set up, basing the input file on that discussed in Section {ref}sec:cookbooks:shell_simple_2d. The full input file can be found at [benchmarks/davies_et_al/case-1.1.prm](https://www.github.com/geodynamics/aspect/blob/main/benchmarks/davies_et_al/case-1.1.prm), with the interesting parts excerpted as follows: {literalinclude} case-1.1.prm  We use the same trick here as in {ref}sec:cookbooks:convection-box to produce a model in which the density $\rho(T)$ in the temperature equation {math:numref}eq:temperature is almost constant (namely, by choosing a very small thermal expansion coefficient) as required by the benchmark, and instead prescribe the desired Rayleigh number by choosing a correspondingly large gravity. Results for this and the other cases are shown below. ## Case 2.1: BA_Ra104_Iso_FS. Case 2.1 uses the following setup, differing only in the boundary conditions: - Boussinesq Approximation - Boundary Condition: Free-Slip - Rayleigh Number = $10^4$ - Initial Conditions: $D = 0, O = 4$ - $\eta(T) = 1$ As a consequence of the free slip boundary conditions, any solid body rotation of the entire system satisfies the Stokes equations with their boundary conditions. In other words, the solution of the problem is not unique: given a solution, adding a solid body rotation yields another solution. We select arbitrarily the one that has no net rotation (see {ref}parameters:Nullspace_20removal). The section in the input file that is relevant is then as follows (the full input file resides at [benchmarks/davies_et_al/case-2.1.prm](https://www.github.com/geodynamics/aspect/blob/main/benchmarks/davies_et_al/case-2.1.prm)): {literalinclude} case-2.1.prm  Again, results are shown below. ## Case 2.2: BA_Ra105_Iso_FS. Case 2.2 is described as follows: - Boussinesq Approximation - Boundary Condition: Free-Slip - Rayleigh Number = $10^5$ - Initial Conditions: Final conditions of case 2.1 (BA_Ra104_Iso_FS) - $\eta(T) = 1$ In other words, we have an increased Rayleigh number and begin with the final steady state of case 2.1. To start the model where case 2.1 left off, the input file of case 2.1, [benchmarks/davies_et_al/case-2.1.prm](https://www.github.com/geodynamics/aspect/blob/main/benchmarks/davies_et_al/case-2.1.prm), instructs to checkpoint itself every few time steps (see {ref}sec:checkpoint-restart). If case 2.2 uses the same output directory, we can then resume the computations from this checkpoint with an input file that prescribes a different Rayleigh number and a later input time: {literalinclude} case-2.2.prm  We increase the Rayleigh number to $10^5$ by increasing the magnitude of gravity in the input file. The full script for case 2.2 is located in [benchmarks/davies_et_al/case-2.2.prm](https://www.github.com/geodynamics/aspect/blob/main/benchmarks/davies_et_al/case-2.2.prm) (sec:benchmarks:davies_et_al:case2.3)= ## Case 2.3: BA_Ra103_vv_FS. Case 2.3 is a variation on the previous one: - Boussinesq Approximation - Boundary Condition: Free-Slip - Rayleigh Number = $10^3$ - Initial Conditions: Final conditions of case 2.1 (BA_Ra104_Iso_FS) - $\eta(T) = 1000^{-T}$ The Rayleigh number is smaller here (and is selected using the gravity parameter in the input file, as before), but the more important change is that the viscosity is now a function of temperature. At the time of writing, there is no material model that would implement such a viscosity, so we create a plugin that does so for us (see {ref}cha:extending and {ref}sec:extending:write-a-plugin in general, and {ref}sec:extending:plugin-types:material-models for material models in particular). The code for it is located in [benchmarks/davies_et_al/case-2.3-plugin/VoT.cc](https://www.github.com/geodynamics/aspect/blob/main/benchmarks/davies_et_al/case-2.3-plugin/VoT.cc) (where "VoT" is short for "viscosity as a function of temperature") and is essentially a copy of the simpler material model. The primary change compared to the simpler material model is the line about the viscosity in the following function: {code-block} c++ template void VoT:: evaluate(const typename Interface::MaterialModelInputs &in, typename Interface::MaterialModelOutputs &out) const { for (unsigned int i=0; i Davies et al. benchmarks: Final steady state temperature fields for the 2D cylindrical benchmark cases.  Secondly, {numref}fig:davies-2DcylinderVrms shows the root mean square velocity as a function of time for the various cases. It is obvious that they all converge to steady state solutions. However, there is an initial transient stage and, in cases 2.2 and 2.3, a sudden jolt to the system at the time where we switch from the model used to compute up to time $t=2$ to the different models used after that. {figure-md} fig:davies-2DcylinderVrms Davies et al. benchmarks: $V_{rms}$ for 2D Cylindrical Cases. Large jumps occur when transitioning from case 2.1 to cases 2.2 and 2.3 due to the instantaneous change of parameter settings.  These runs also produce quantitative data that will be published along with the concise descriptions of the benchmarks and a comparison with other codes. In particular, some of the criteria listed above to judge the accuracy of results are listed in {numref}tab:davies-et-al-results.[^footnote1] {table} Davies et al. benchmarks: Numerical results for some of the output quantities required by the benchmarks and the various cases considered. :name: tab:davies-et-al-results | Case | $\left$ | $Nu_T$ | $Nu_B$ | $V_{\text{rms}}$ | |:-----|:----------------:|:------:|:------:|:----------------:| | 1.1 | 0.403 | 2.464 | 2.468 | 19.053 | | 2.1 | 0.382 | 4.7000 | 4.706 | 46.244 | | 2.2 | 0.382 | 9.548 | 9.584 | 193.371 | | 2.3 | 0.582 | 5.102 | 5.121 | 79.632 |  [^footnote1]: The input files available in the benchmarks/davies_et_al directory use 5 global refinements in order to provide cases that can be run without excessive trouble on a normal computer. However, this is not enough to achieve reasonable accuracy and both the data shown below and the data submitted to the benchmarking effort uses 7 global refinement steps, corresponding to a mesh with 1536 cells in tangential and 128 cells in radial direction. Computing on such meshes is not cheap, as it leads to a problem size of more than 2.5 million unknowns. It is best done using a parallel computation.