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Mesoscale Subduction at the Antarctic Polar Front Driven by Baroclinic Instability
Mesoscale Subduction Antarctic Polar Front Driven Baroclinic Instability
2008/8/7
A study of mesoscale subduction at the Antarctic Polar Front (PF) is conducted by use of hydrographic data from a high-resolution, quasi-synoptic survey of the front. The geostrophic velocity and isop...