Submesoscale frontal dynamics modulate ocean heat 1 transport beneath Antarctic sea ice 2
L. Siegelman, Andrew F. Thompson, C. Dupin et al.
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Open access
Aug 2026
Meso- and Sub-mesoscale Wind–Front Interactions and Their Impacts on Ocean Vertical Velocities
Coherent surface ocean temperature and velocity structures, with scales spanning 10–100 km, induce surface wind stress anomalies that generate near-surface vertical velocities through Ekman dynamics. These wind–front interactions are known as Thermal (TFB) and Current (CFB) feedbacks. Their relative contributions t...
Yue Bai, Andrew F. Thompson, A. B. Villas Boas et al.
· Journal of Physical Oceanogr... · 0 citations