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Oceanic Frontal Turbulence
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2024
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Source: Journal of Physical Oceanography, 54(2), 333-358
[PDF-11.62 MB]
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Journal Title:Journal of Physical Oceanography
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Description:Upper-ocean turbulence results from a complex set of interactions between submesoscale turbulence and local boundary layer processes. The interaction between larger-scale currents and turbulent fluctuations is two-way: large-scale shearing motions generate turbulence, and the resulting coherent turbulent fluxes of momentum and buoyancy feed back onto the larger flow. Here we examine the evolution and role of turbulence in the intensification, instability, arrest, and decay (i.e., the life cycle) of a dense filament undergoing frontogenesis in the upper-ocean boundary layer, i.e., cold filament frontogenesis (CFF).
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Source:Journal of Physical Oceanography, 54(2), 333-358
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ISSN:0022-3670;1520-0485;
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