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    Observations of the Transition Layer 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 003:;page 780
    Author(s): Johnston, T. M. Shaun; Rudnick, Daniel L.
    Publisher: American Meteorological Society
    Abstract: The transition layer is the poorly understood interface between the stratified, weakly turbulent interior and the strongly turbulent surface mixed layer. The transition layer displays elevated thermohaline variance compared ...
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    Interannual Geostrophic Current Anomalies in the Near-Equatorial Western Pacific 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 001:;page 3
    Author(s): Johnston, T. M. Shaun; Merrifield, Mark A.
    Publisher: American Meteorological Society
    Abstract: A network of island tide gauges is used to estimate interannual geostrophic current anomalies (GCAs) in the western Pacific from 1975 to 1997. The focus of this study is the zonal component of the current averaged between ...
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    Standing Internal Tides in the Tasman Sea Observed by Gliders 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 011:;page 2715
    Author(s): Johnston, T. M. Shaun; Rudnick, Daniel L.; Kelly, Samuel M.
    Publisher: American Meteorological Society
    Abstract: ow-mode internal tides are generated at tall submarine ridges, propagate across the open ocean with little attenuation, and reach distant continental slopes. A semidiurnal internal tide beam, identified in previous altimetric ...
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    Interference Pattern and Propagation of the M2 Internal Tide South of the Hawaiian Ridge 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 002:;page 311
    Author(s): Rainville, Luc; Johnston, T. M. Shaun; Carter, Glenn S.; Merrifield, Mark A.; Pinkel, Robert; Worcester, Peter F.; Dushaw, Brian D.
    Publisher: American Meteorological Society
    Abstract: Most of the M2 internal tide energy generated at the Hawaiian Ridge radiates away in modes 1 and 2, but direct observation of these propagating waves is complicated by the complexity of the bathymetry at the generation ...
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    The Equatorial Current System West of the Galápagos Islands during the 2014–16 El Niño as Observed by Underwater Gliders 

    Source: Journal of Physical Oceanography:;2021:;volume( 051 ):;issue: 001:;page 3
    Author(s): Rudnick, Daniel L.;Owens, W. Brechner;Johnston, T. M. Shaun;Karnauskas, Kristopher B.;Jakoboski, Julie;Todd, Robert E.
    Publisher: American Meteorological Society
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    Flippin’ χSOLO, an Upper-Ocean Autonomous Turbulence-Profiling Float 

    Source: Journal of Atmospheric and Oceanic Technology:;2023:;volume( 040 ):;issue: 005:;page 629
    Author(s): Moum, James N.; Rudnick, Daniel L.; Shroyer, Emily L.; Hughes, Kenneth G.; Reineman, Benjamin D.; Grindley, Kyle; Sherman, Jeffrey T.; Vutukur, Pavan; Appledorn, Craig Van; Latham, Kerry; Moulin, Aurélie J.; Johnston, T. M. Shaun
    Publisher: American Meteorological Society
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