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    Systematic Bias in Baroclinic Energy Estimates in Shelf Seas 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 009:;page 2851
    Author(s): Stephenson, Gordon R.; Green, J. A. Mattias; Inall, Mark E.
    Publisher: American Meteorological Society
    Abstract: simple model of an internal wave advected by an oscillating barotropic flow suggests flaws in standard approaches to estimating properties of the internal tide. When the M2 barotropic tidal current amplitude is of similar ...
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    Measurement of the Rates of Production and Dissipation of Turbulent Kinetic Energy in an Energetic Tidal Flow: Red Wharf Bay Revisited 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 009:;page 1889
    Author(s): Rippeth, Tom P.; Simpson, John H.; Williams, Eirwen; Inall, Mark E.
    Publisher: American Meteorological Society
    Abstract: Simultaneous measurements of the rates of turbulent kinetic energy (TKE) dissipation (ε) and production (P) have been made over a period of 24 h at a tidally energetic site in the northern Irish Sea in water of 25-m depth. ...
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    Overturning in the Subpolar North Atlantic Program: A New International Ocean Observing System 

    Source: Bulletin of the American Meteorological Society:;2016:;volume( 098 ):;issue: 004:;page 737
    Author(s): Susan Lozier, M.; Bacon, Sheldon; Bower, Amy S.; Cunningham, Stuart A.; Femke de Jong, M.; de Steur, Laura; deYoung, Brad; Fischer, Jürgen; Gary, Stefan F.; Greenan, Blair J. W.; Heimbach, Patrick; Holliday, Naomi P.; Houpert, Loïc; Inall, Mark E.; Johns, William E.; Johnson, Helen L.; Karstensen, Johannes; Li, Feili; Lin, Xiaopei; Mackay, Neill; Marshall, David P.; Mercier, Herlé; Myers, Paul G.; Pickart, Robert S.; Pillar, Helen R.; Straneo, Fiammetta; Thierry, Virginie; Weller, Robert A.; Williams, Richard G.; Wilson, Chris; Yang, Jiayan; Zhao, Jian; Zika, Jan D.
    Publisher: American Meteorological Society
    Abstract: or decades oceanographers have understood the Atlantic meridional overturning circulation (AMOC) to be primarily driven by changes in the production of deep-water formation in the subpolar and subarctic North Atlantic. ...
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