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    Shear at the Base of the Oceanic Mixed Layer Generated by Wind Shear Alignment 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 008:;page 1798
    Author(s): Brannigan, Liam; Lenn, Yueng-Djern; Rippeth, Tom P.; McDonagh, Elaine; Chereskin, Teresa K.; Sprintall, Janet
    Publisher: American Meteorological Society
    Abstract: bservations are used to evaluate a simple theoretical model for the generation of near-inertial shear spikes at the base of the open ocean mixed layer when the upper ocean displays a two-layer structure. The model predicts ...
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    Submesoscale Instabilities in Mesoscale Eddies 

    Source: Journal of Physical Oceanography:;2017:;Volume( 047 ):;issue: 012:;page 3061
    Author(s): Brannigan, Liam;Marshall, David P.;Naveira Garabato, Alberto C.;Nurser, A. J. George;Kaiser, Jan
    Publisher: American Meteorological Society
    Abstract: AbstractSubmesoscale processes have been extensively studied in observations and simulations of fronts. Recent idealized simulations show that submesoscale instabilities also occur in baroclinic mesoscale cyclones and ...
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    An Annual Cycle of Submesoscale Vertical Flow and Restratification in the Upper Ocean 

    Source: Journal of Physical Oceanography:;2019:;volume 049:;issue 006:;page 1439
    Author(s): Yu, Xiaolong; Naveira Garabato, Alberto C.; Martin, Adrian P.; Buckingham, Christian E.; Brannigan, Liam; Su, Zhan
    Publisher: American Meteorological Society
    Abstract: AbstractNumerical simulations suggest that submesoscale turbulence may transform lateral buoyancy gradients into vertical stratification and thus restratify the upper ocean via vertical flow. However, the observational ...
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