Coherent dipoles in a mixed layer with variable buoyancy: Theory compared to observations

Noé Lahaye (1, 2) , Vladimir Zeitlin (3, 4) , Thomas Dubos (3)

1 FLUMINANCE - Fluid Flow Analysis, Description and Control from Image Sequences
2 LOPS - Laboratoire d'Océanographie Physique et Spatiale
3 LMD - Laboratoire de Météorologie Dynamique (UMR 8539)
4 SUSTech - Southern University of Science and Technology

Motivated by recent observations of coherent dipolar cyclone-anticyclone structures in the ocean, the modons, and their signature in the surface temperature field, we demonstrate that the classical modon solutions of the barotropic quasi-geostrophic equations can be generalized to include buoyancy or temperature as an active tracer. The properties of such "thermal" modons, and especially their ability to carry heat anomaly over long distances, depend on the relative sign of the associated vorticity and buoyancy anomalies. We show using numerical simulations with the thermal shallow water equations, and their quasi-geostrophic version, that the evolution of the modons is consistent with the observations.

Domaines: Océan, Atmosphère; Mécanique des fluides [physics.class-ph]; Météorologie; Océanographie

Noé Lahaye, Vladimir Zeitlin, Thomas Dubos. Coherent dipoles in a mixed layer with variable buoyancy: Theory compared to observations. Ocean Modelling, 2020, 153, pp.101673. ⟨10.1016/j.ocemod.2020.101673⟩. ⟨hal-03006503⟩