Wind blows, water moves.
Ellipse and circle, their paths,
noose-like, strangle me.
University of North Carolina at Chapel Hill
In the Georgia Bight, near 30 degrees North, the local inertial period is close to 24 hours, and sea breeze/land breeze wind forcing and the forced response in the coastal ocean come into resonance. My dissertation work examined the structure and variability of both sea breeze/land breeze and the coastal ocean response, as well as the processes that control the horizontal and vertical structures of the near-resonant diurnal/inertial currents.
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