Symmetry breaking and nonlinear transformation of two-layer eastward propagating dipoles

TL;DR

This paper investigates the evolution and symmetry breaking of eastward propagating dipoles in a two-layer quasi-geostrophic model, revealing mechanisms of instability, nonlinear transformation, and the formation of long-lived asymmetric dipoles.

Contribution

It uncovers the nonlinear transformation phases of dipoles, the role of the upper layer β-effect in symmetry breaking, and introduces a new type of long-lived dipole with weak Rossby wave radiation.

Findings

Symmetry breaks due to an exponentially-growing asymmetric Rossby wave mode.

Nonlinear transformation involves fast partner separation and slow asymmetric mode development.

Weakly radiating long-lived dipoles form with homogenized potential vorticity.

Abstract

We study the evolution of eastward propagating dipoles (modons) in a two-layer quasi-geostrophic $\beta$-plane model using high-resolution numerical simulations. Various combinations of background gradients of potential vorticity in the upper and lower layer (which may include sloping topography) shed light on the recently discovered breakdown mechanisms and rich dynamics of dipolar vortices. Owing to the $\beta$-effect in the upper layer with active dipolar vortices, the symmetry of the dipole flow breaks due to an exponentially-growing, rotating, asymmetric mode of linear instability associated with Rossby wave radiation. Further nonlinear transformation is found to consist of two phases: fast partner separation, resulting in a deceleration of the eastward drift, and subsequent slow separation with a saturated asymmetric mode accompanied by much weaker, shorter Rossby waves. This weakly radiating phase -- with pulsating partners and homogenized potential vorticity between the core and the separatrix -- can be considered as a new type of long-lived dipole. Conversely, when no $\beta$-effect is present in the upper layer, the dipoles remain nearly symmetric, even when the topographic $\beta$-effect is present in the active lower layer. In this case, the development of a weak asymmetric mode is related to a small meridional shift of the dipole center on the numerical grid.