Hot Jupiters are Inflated Primarily by Shallow Heating
Stephen P. Schmidt, Daniel P. Thorngren, Kevin C. Schlaufman
TL;DR
This paper addresses the hot Jupiter radius inflation problem by developing a thermal evolution model that combines deep interior heating with delayed cooling, allowing for substantial shallow heating near the radiative-convective boundary. Using a homogeneous, self-consistent catalog of host-star and planetary properties, the authors apply a two-level hierarchical Bayesian framework to infer population-level heating parameters, marginalizing over planet-specific properties. They find that interior cooling is reduced by roughly a factor of 20–60 compared with deep-heating-only models, implying that shallow heating accounts for the majority of inflation (roughly 95–97% of the heating) and enabling reinflation with modest deep heating. The results favor shallow heating mechanisms such as Ohmic dissipation and advection, with testable predictions for phase curve offsets as a function of equilibrium temperature, and they emphasize the importance of incorporating shallow heating in atmospheric and circulation models for hot Jupiters.
Abstract
The unexpectedly large radii of transiting hot Jupiters have led to many proposals for the physical mechanisms responsible for heating their interiors. While it has been shown that hot Jupiters reinflate as their host stars brighten due to heating deep in planetary interiors, young hot Jupiters also exhibit signs of delayed cooling possibly related to heating closer to their surfaces. To investigate this tension, we enhance our previously published hot Jupiter thermal evolution model by adding a parameter that allows for both deep heating and delayed cooling. We fit our thermal evolution models to a homogeneous, physically self-consistent catalog of accurate and precise hot Jupiter system properties in a hierarchical Bayesian framework. We find that hot Jupiters' interior cooling rates are reduced on average by 95\%--98\% compared to simpler anomalous heating models. The most plausible explanation for this inference is substantial shallow heating just below their radiative--convective boundaries that enables reinflation with much less deep heating. Shallow heating by Ohmic dissipation and/or temperature advection are therefore important components of accurate models of hot Jupiter atmospheres, especially in circulation models. If hot Jupiters are inflated primarily by shallow heating as we propose, then we predict that their observed phase curve offsets should increase with temperature in the range $T_{\text{eq}}~\lesssim1500~\text{K}$, peak in the range $1500~\text{K}~\lesssim~T_{\text{eq}}~\lesssim~1800~\text{K}$, and decrease in the range $T_{\text{eq}}~\gtrsim~1800~\text{K}$.
