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1 Introduction Submesoscale ocean motions, characterized by length scales small compared to the deformation radius and possessing O ( 1 ) $O(1)$ -Rossby numbers, are ubiquitous across the global ocean surface and play an important role in setting the vertical structure and energy budget of the upper ocean (Su et al., 2018; Taylor & Thompson, 2023).
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1 Introduction The global meridional overturning circulation (MOC) plays a central role in Earth's climate, modulating the exchange of watermasses between the surface and the deep ocean and facilitating a large portion of the world's heat transport and carbon dioxide uptake (Ferrari & Ferreira, 2011; Toggweiler et al., 2006). The MOC is often described in terms of two circulation cells: the mid-depth cell and the abyssal cell.
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