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The Heton, an Elementary Interaction Between Discrete Baroclinic Geostrophic Vortices, and Its Implications Concerning Eddy Heat-Flow

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TLDR
In this article, a simple two-heton engine that exhibits vortex splitting, loss of available potential energy, and meridional heat transport is presented, which is a simplified version of the one presented in this paper.
Abstract
Among the interactions of two discrete baroclinic geostrophic vortices in a two-layer system there is one class of interaction that is non-trivial; when the two vortices are of opposite sign and in different layers, and close enough together, they transport heat. Because this particular interaction can transport heat, we propose to call it the heton. It is a tilted baroclinic pair. In the Northern Hemisphere it transports heat to the left of the direction toward which its top tilts. Two warm or two cold hetons repel one another when outside the radius of deformation. A warm and a cold heton attract one another. A simple two-heton engine that exhibits vortex splitting, loss of available potential energy, and meridional heat transport is presented.

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Vortices in Rotating Fluids

TL;DR: The emergence of coherent vortex structures is a characteristic feature of quasi-geostrophic or two-dimensional turbulence and because of their relevance to large-scale geophysical flows, the dynamics of these structures has been studied increasingly over the past decade.
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Statistical mechanics of two-dimensional and geophysical flows

TL;DR: In this article, the authors present a review of the theoretical study of the self-organization of two-dimensional and geophysical turbulent flows, from the statistical mechanics basis of the theory up to applications to Jupiter troposphere and ocean vortices and jets.
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The Cape Cauldron: A regime of turbulent inter-ocean exchange

TL;DR: In this paper, the Lagrangian intermediate depth velocity measurements from the KAPEX (Cape of Good Hope Experiments) float program with sea-surface height data were combined with sea surface height data to study the inter-ocean exchange mechanisms around southern Africa.
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Isolated Eddy Models in Geophysics

TL;DR: In the Earth's ocean, we find similar long-lived structures, e.g., Gulf Stream rings as mentioned in this paper, that can progress over thousands of kilometers. But, because of the extremely active role of the thermodynamic proces, these properties may require quite different explanations.
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Western Arctic Shelfbreak Eddies : Formation and Transport

TL;DR: In this article, the mean structure and time-dependent behavior of the shelf break jet along the southern Beaufort Sea, and its ability to transport properties into the basin interior via eddies are explored using high-resolution mooring data and an idealized numerical model.
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