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    Mixing Structure of High-Frequency Internal Waves in the Upper EasternEquatorial Pacific 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 012:;page 3090
    Author(s): Mack, Andrew P.; Hebert, D.
    Publisher: American Meteorological Society
    Abstract: A thermistor chain towed from 140° to 110°W along the equator revealed the presence of high-frequency internal waves in the upper 125 m having zonal wavelengths of 150?250 m. Turbulence dissipation rates, ε, observed from ...
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    The Cross-Stream Potential Vorticity Front and Its Role in Meander-Induced Exchange in the Gulf Stream 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 012:;page 3551
    Author(s): Rajamony, J.; Hebert, D.; Rossby, T.
    Publisher: American Meteorological Society
    Abstract: The potential vorticity (PV) front observed in the upper thermocline at the northern edge of the Gulf Stream has been thought of as an inhibitor to lateral motion of parcels on isopycnals. The role of the PV front in ...
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    Estimating Lagrangian Trajectories with an ADCP 

    Source: Journal of Atmospheric and Oceanic Technology:;1999:;volume( 016 ):;issue: 009:;page 1255
    Author(s): Rajamony, J.; Hebert, D.; Rossby, T.
    Publisher: American Meteorological Society
    Abstract: Lagrangian trajectories may be estimated with an Acoustic Doppler Current Profiler (ADCP) as an alternative to tracking parcels with floats. By using the depth of isopycnals from a conductivity?temperature?depth (CTD) ...
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    Does Ocean Turbulence Peak at the Equator?: Revisited 

    Source: Journal of Physical Oceanography:;1991:;Volume( 021 ):;issue: 011:;page 1690
    Author(s): Hebert, D.; Moum, J. N.; Caldwell, D. R.
    Publisher: American Meteorological Society
    Abstract: In spite of the effects of several form of temporal variability that tend to mask geographical patterns in turbulence intensity, our evidence indicates that the turbulence is enhanced above the equatorial undercurrent in ...
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    Turbulence and Internal Waves at the Equator. Part I: Statistics from Towed Thermistors and a Microstructure Profiler 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 011:;page 1330
    Author(s): Moum, J. N.; Hebert, D.; Paulson, C. A.; Caldwell, D. R.
    Publisher: American Meteorological Society
    Abstract: High correlations between turbulent dissipation rates and high-wavenumber internal waves and the high values of turbulent dissipation associated with internal wave activity suggest that internal waves are the main direct ...
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    Turbulence and Internal Waves at the Equator. Part II: Details of a Single Event 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 011:;page 1346
    Author(s): Hebert, D.; Moum, J. N.; Paulson, C. A.; Caldwell, D. R.
    Publisher: American Meteorological Society
    Abstract: In the low Richardson number shear flow above the Pacific Equatorial Undercurrent, a single vertical microstructure profile intersected the overturning crest of a packet of high horizontal wavenumber waves. The observed ...
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    Universality of the Modeled Small-Scale Response of the Upper Tropical Ocean to Squall Wind Forcing 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 003:;page 519
    Author(s): Richardson, R. A.; Sutyrin, G. G.; Hebert, D.; Rothstein, L. M.
    Publisher: American Meteorological Society
    Abstract: The upper ocean response to idealized surface wind forcing that is representative of conditions observed during the TOGA-COARE Intensive Observation Period is studied by numerical simulations using a second-moment closure ...
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    Internal Waves, Dynamic Instabilities, and Turbulence in the Equatorial Thermocline: An Introduction to Three Papers in this Issue 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 011:;page 1357
    Author(s): Moum, J. N.; Hebert, D.; Paulson, C. A.; Caldwell, D. R.; McPhaden, M. J.; Peters, H.
    Publisher: American Meteorological Society
    Abstract: Appearing in this issue of the Journal of Physical Oceanography are three papers that present new observations of a distinct, narrow band, and diurnally varying signal in temperature records obtained in the low Richardson ...
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