<p>Super-Earths are by far the most dominant type of exoplanet, yet their formation is<br />still not well understood. In particular, planet formation models predict that many<br />of them should have accreted enough gas to become gas giants. Here we examine the<br />role of the protoplanetary disk in the cooling and contraction of the protoplanetary<br />envelope. In particular, we investigate the effects of 1) the thermal state of the disk as<br />set by the relative size of heating by accretion or irradiation, and whether its energy is<br />transported by radiation or convection, and 2) advection of entropy into the outer envelope by disk flows that penetrate the Hill sphere, as found in 3D global simulations.<br />We find that, at 0.1 AU, the envelope quickly becomes fully radiative, nearly isothermal, and thus cannot cool down, stalling gas accretion. This<br />effect is significantly more pronounced in convective disks, leading to envelope mass or-<br />ders of magnitude lower. Entropy advection at 0.1 AU in either radiative or convective<br />disks could therefore explain why super-Earths failed to undergo runaway accretion.</p>
<p>Ali-Dib, Cumming, & Lin (MNRAS 2020)</p>