Spherical convective dynamo with solar rotation rate: The rotation in the reference frame is Omega0=2.70000e-06 1/s The azimuthal velocity gives the difference reference frame, so positive values = faster rotation than the reference frame and vice versa. For these slow rotation rate the run develops a so called anti-solar differential rotation, where the equator rotates slower than the poles. The magnetic field is in this case rather constant with no clear cyles. The time resolution is around 13.8 days and the whole data set spanns around 94.7 years For numerical reasons, we have to leave out the poles, so we cut the last 15 degrees. The simulation spans from 0.7 to 1.0 in radius, but the density stratification is not realistic. Please find the overview of the quantites contained in the fit files: nr: number of radial grid points ntheta: number of latitudinal grid points ntime : number of points in time ncomp : components, with radial, latitudinal, azimuthal direction File structure units magnetic_field [nr,ntheta,ntime,ncomp] Gauss velocity_field [nr,ntheta,ntime,ncomp] m/s sound_speed [nr,ntheta,ntime] m/s density [nr,ntheta,ntime] kg/m3 time [ntime] s radius [nr] m theta [ntheta] rad (Colatitude: theta=0 -> north pole) More information about these models can be found in: Warnecke, J. and Kapyla, M. J.,: 2020, Rotational dependence of turbulent transport coefficients in global convective dynamo simulations of solar-like stars, Astron. Astrophys., accepted, arXiv: 1910.06776 Warnecke, J.: 2018, Dynamo cycles in global convection simulations of solar-like stars, Astron. Astrophys., 616, A72 Kapyla, P. J., Mantere, M. J., Cole, E., Warnecke, J., & Brandenburg, A.: 2013, Effects of strong stratification on equatorward dynamo wave propagation, Astrophys. J., 778, 41.