Fig. 6From: Extremely long transition phase of thermal convection in the mantle of massive super-EarthsThe gradient of horizontally averaged temperature −(dT ave/dz) (red curves), the adiabatic temperature gradient calculated from −(dT ave/dz)ad = \(\alpha \cdot Di \cdot T_{\text{ave}}\) (blue curves, both left column), and the horizontally averaged RMS velocity (right column), all plotted against height z at various timesBack to article page