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    Vertical Motion of Neutrally Buoyant Floats 

    Source: Journal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 001:;page 38
    Author(s): Goodman, Louis; Levine, Edward R.
    Publisher: American Meteorological Society
    Abstract: The vertical motion of a neutrally buoyant float is determined from the solution to the nonlinear forced harmonic oscillator equation originally set forth by Voorhis. Float response to forced vertical oscillations is ...
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    On Measuring the Terms of the Turbulent Kinetic Energy Budget from an AUV 

    Source: Journal of Atmospheric and Oceanic Technology:;2006:;volume( 023 ):;issue: 007:;page 977
    Author(s): Goodman, Louis; Levine, Edward R.; Lueck, Rolf G.
    Publisher: American Meteorological Society
    Abstract: The terms of the steady-state, homogeneous turbulent kinetic energy budgets are obtained from measurements of turbulence and fine structure from the small autonomous underwater vehicle (AUV) Remote Environmental Measuring ...
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    The LatMix Summer Campaign: Submesoscale Stirring in the Upper Ocean 

    Source: Bulletin of the American Meteorological Society:;2014:;volume( 096 ):;issue: 008:;page 1257
    Author(s): Shcherbina, Andrey Y.; Sundermeyer, Miles A.; Kunze, Eric; D’Asaro, Eric; Badin, Gualtiero; Birch, Daniel; Brunner-Suzuki, Anne-Marie E. G.; Callies, Jörn; Kuebel Cervantes, Brandy T.; Claret, Mariona; Concannon, Brian; Early, Jeffrey; Ferrari, Raffaele; Goodman, Louis; Harcourt, Ramsey R.; Klymak, Jody M.; Lee, Craig M.; Lelong, M.-Pascale; Levine, Murray D.; Lien, Ren-Chieh; Mahadevan, Amala; McWilliams, James C.; Molemaker, M. Jeroen; Mukherjee, Sonaljit; Nash, Jonathan D.; Özgökmen, Tamay; Pierce, Stephen D.; Ramachandran, Sanjiv; Samelson, Roger M.; Sanford, Thomas B.; Shearman, R. Kipp; Skyllingstad, Eric D.; Smith, K. Shafer; Tandon, Amit; Taylor, John R.; Terray, Eugene A.; Thomas, Leif N.; Ledwell, James R.
    Publisher: American Meteorological Society
    Abstract: ateral stirring is a basic oceanographic phenomenon affecting the distribution of physical, chemical, and biological fields. Eddy stirring at scales on the order of 100 km (the mesoscale) is fairly well understood and ...
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