The Equatorial Jet Speed on Tidally Locked Planets: I -- Terrestrial Planets

TL;DR

This paper develops a predictive theory for the formation of superrotating equatorial jets on tidally locked terrestrial planets, based on stationary wave interactions and validated through models and GCM simulations.

Contribution

It introduces a new mechanism explaining jet formation on terrestrial tidally locked planets, supported by a hierarchy of models and GCM validation.

Findings

Stationary waves induce equatorial acceleration.

The jet is balanced by vertical atmospheric motion.

The simple model estimates jet speed effectively.

Abstract

The atmospheric circulation of tidally locked planets is dominated by a superrotating eastward equatorial jet. We develop a predictive theory for the formation of this jet, proposing a mechanism in which the three-dimensional stationary waves induced by the day-night forcing gradient produce an equatorial acceleration. This is balanced in equilibrium by an interaction between the resulting jet and the vertical motion of the atmosphere. The three-dimensional structure of the zonal acceleration is vital to this mechanism. We demonstrate this mechanism in a hierarchy of models. We calculate the three-dimensional stationary waves induced by the forcing on these planets, and show the vertical structure of the zonal acceleration produced by these waves, which we use to suggest a mechanism for how the jet forms. GCM simulations are used to confirm the equilibrium state predicted by this mechanism, where the acceleration from these waves is balanced by an interaction between the zonal-mean vertical velocity and the jet. We derive a simple model of this using the "Weak Temperature Gradient" approximation, which gives an estimate of the jet speed on a terrestrial tidally locked planet. We conclude that the proposed mechanism is a good description of the formation of an equatorial jet on a terrestrial tidally locked planet, and should be useful for interpreting observations and simulations of these planets. The mechanism requires assumptions such as a large equatorial Rossby radius and weak acceleration due to transient waves, and a different mechanism may produce the equatorial jets on gaseous tidally locked planets.