Abstract

Context. Atmospheric superrotating flows at the equator are a nearly ubiquitous result when conducting simulations of hot Jupiters. One theory explaining how this zonally-coherent flow reaches equilibrium has already been developed in the literature. This understanding, however, relies on the existence of either an initial superrotating flow or a sheared flow, coupled with a slow evolution that permits a linear steady state to be reached. Aims. A consistent physical understanding of superrotation is needed for arbitrary drag and radiative timescales, along with the relevance of taking linear steady states into account, needs to be assessed. Methods. We obtained an analytical expression for the structure, frequency, and decay rate of propagating waves in hot Jupiter atmospheres around a state at rest in the 2D shallow-water β-plane limit. We solved this expression numerically and confirmed the robustness of our results with a 3D linear wave algorithm. We then compared it with 3D simulations of hot Jupiter atmospheres and studied the nonlinear momentum fluxes. Results. We show that under strong day-night heating, the dynamics do not transit through a linear steady state when starting from an initial atmosphere in solid body rotation. We further demonstrate that nonlinear effects favor the initial spin-up of superrotation and that acceleration due to the vertical component of the eddy-momentum flux is critical to the initial development of superrotation. Conclusions. We describe the initial phases of the acceleration of superrotation, including the consideration of differing radiative and drag timescales, and we conclude that eddy-momentum-driven superrotating equatorial jets are robust, physical phenomena in simulations of hot Jupiter atmospheres.

Highlights

  • Understanding the atmospheric dynamics of hot Jupiters, which are Jovian planets in short-period orbits, has been a major challenge since their discovery (Mayor & Queloz 1995)

  • We obtained an analytical expression for the structure, frequency, and decay rate of propagating waves in hot Jupiter atmospheres around a state at rest in the 2D shallow-water β-plane limit

  • We show that under strong day-night heating, the dynamics do not transit through a linear steady state when starting from an initial atmosphere in solid body rotation

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Summary

Introduction

Understanding the atmospheric dynamics of hot Jupiters, which are Jovian planets in short-period orbits, has been a major challenge since their discovery (Mayor & Queloz 1995). Tsai et al (2014) extend the study to a full 3D dynamical model and include a consideration of the resonance of the atmospheric wave response, as well as the “tilt” of the vertical component which acts to drive the vertical eddy-momentum transport, under the assumption of equal drag and radiative timescales. This is followed by Hammond & Pierrehumbert (2018), who explore superrotation in 2D with the addition of a shearing flow. Our study shows that the paradigm of equatorial superrotation in hot Jupiters is robust: superrotation is accelerated by an eddy-mean flow interaction (i.e., atmospheric waves interacting with the background flow) and it is strongly influenced by the wave-dissipation timescales and vertical momentum convergence

Solution to 2D shallow water equations
Time-dependent solutions
Insensitivity of the Matsuno–Gill solution to differential heating
Decay time of damped waves
Rossby waves
Kelvin waves
Decay timescale summary
Qualitative structure of linear steady state
Order-of-magnitude analysis
Conclusion
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