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    Air–Sea Heat Flux Measurements from Nearly Neutrally Buoyant Floats 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 007:;page 1086
    Author(s): D'Asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: The ability of neutrally buoyant, high-drag floats to measure the air?sea heat flux from within the turbulent oceanic boundary layer is investigated using float data from four different winter and fall float deployments. ...
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    Estimation of Velocity from Argos-tracked Surface Drifters during OCEAN STORMS 

    Source: Journal of Atmospheric and Oceanic Technology:;1992:;volume( 009 ):;issue: 005:;page 680
    Author(s): D'Asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: Modern surface drifters tracked by Argos are an attractive method for measuring the spatial structure of near-surface currents. This note discusses the accuracy to which velocity can be estimated from such data, assuming ...
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    Upper-Ocean Inertial Currents Forced by a Strong Storm. Part II: Modeling 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 011:;page 2937
    Author(s): D'asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: The evolution of near-inertial frequency currents is often thought to be controlled by the linear, inviscid equations of motion. This hypothesis is tested by simulating the near-inertial currents described in Part I using ...
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    Upper-Ocean Inertial Currents Forced by a Strong Storm. Part III: Interaction of Inertial Currents and Mesoscale Eddies 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 011:;page 2953
    Author(s): D'asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: The interaction of strong near-inertial frequency currents generated by a storm with preexisting subinertial frequency currents is investigated. For 10 days after the storm, the near-inertial currents remain in the mixed ...
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    Turbulent Vertical Kinetic Energy in the Ocean Mixed Layer 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 012:;page 3530
    Author(s): D'Asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: Vertical velocities in the ocean boundary layer were measured for two weeks at an open ocean, wintertime site using neutrally buoyant floats. Simultaneous measurements of the surface meteorology and surface waves showed a ...
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    The Ocean Boundary Layer below Hurricane Dennis 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 003:;page 561
    Author(s): D'Asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: Three neutrally buoyant floats were air deployed ahead of Hurricane Dennis on 28 August 1999. These floats were designed to accurately follow three-dimensional water trajectories and measure pressure (i.e., their own depth) ...
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    The Energy Flux from the Wind to Near-Inertial Motions in the Surface Mixed Layer 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 008:;page 1043
    Author(s): D'Asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: Time series of wind stress computed from long-term meteorological buoy data off North America are used to examine the forcing of surface inertial currents by the wind. A simple damped slab model of the mixed layer is used ...
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    Upper Ocean Temperature Structure, Inertial Currents, and Richardson Numbers Observed during Strong Meteorological Forcing 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 007:;page 943
    Author(s): D'Asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: Upper ocean currents and temperature in the northeastern Pacific were measured during a 14-day period in November 1980 as part of STREX. Velocities in the upper ocean are dominated by near-inertial frequency oscillations. ...
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    Performance of Autonomous Lagrangian Floats 

    Source: Journal of Atmospheric and Oceanic Technology:;2003:;volume( 020 ):;issue: 006:;page 896
    Author(s): D'Asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: A truly Lagrangian float would follow all three components of oceanic velocity on all timescales. Progress toward this goal is reviewed by analyzing the performance of nearly Lagrangian floats deployed in a variety of ...
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    Solar Power for Autonomous Floats 

    Source: Journal of Atmospheric and Oceanic Technology:;2007:;volume( 024 ):;issue: 007:;page 1309
    Author(s): D’Asaro, Eric A.
    Publisher: American Meteorological Society
    Abstract: Advances in low-power instrumentation and communications now often make energy storage the limiting factor for long-term autonomous oceanographic measurements. Recent advances in photovoltaic cells, with efficiencies now ...
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