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    Loop Current and Deep Eddies 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 007:;page 1426
    Author(s): Oey, L-Y.
    Publisher: American Meteorological Society
    Abstract: In contrast to the Loop Current and rings, much less is known about deep eddies (deeper than 1000 m) of the Gulf of Mexico. In this paper, results from a high-resolution numerical model of the Gulf are analyzed to explain ...
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    Coupled Response of the Trade Wind, SST Gradient, and SST in the Caribbean Sea, and the Potential Impact on Loop Current's Interannual Variability 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 007:;page 1325
    Author(s): Chang, Y.-L.; Oey, L.-Y.
    Publisher: American Meteorological Society
    Abstract: ir?sea coupling in the IntraAmerican seas (IAS; Caribbean Sea and Gulf of Mexico) is studied through analyses of observational data from satellite, reanalysis products, and in situ measurements. A strong coupling is found ...
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    Instability of the North Pacific Subtropical Countercurrent 

    Source: Journal of Physical Oceanography:;2013:;Volume( 044 ):;issue: 003:;page 818
    Author(s): Chang, Y.-L.; Oey, L.-Y.
    Publisher: American Meteorological Society
    Abstract: he North Pacific Subtropical Countercurrent (STCC) has a weak eastward velocity near the surface, but the region is populated with eddies. Studies have shown that the STCC is baroclinically unstable with a peak growth rate ...
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    Loop Current Growth and Eddy Shedding Using Models and Observations: Numerical Process Experiments and Satellite Altimetry Data 

    Source: Journal of Physical Oceanography:;2012:;Volume( 043 ):;issue: 003:;page 669
    Author(s): Chang, Yu-Lin; Oey, L.-Y.
    Publisher: American Meteorological Society
    Abstract: ecent studies on Loop Current?s variability in the Gulf of Mexico suggest that the system may behave with some regularity forced by the biannually varying trade winds. The process is analyzed here using a reduced-gravity ...
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    CORRIGENDUM 

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 008:;page 2248
    Author(s): Chang, Y.-L.; Oey, L.-Y.
    Publisher: American Meteorological Society
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    The Philippines–Taiwan Oscillation: Monsoonlike Interannual Oscillation of the Subtropical–Tropical Western North Pacific Wind System and Its Impact on the Ocean 

    Source: Journal of Climate:;2011:;volume( 025 ):;issue: 005:;page 1597
    Author(s): Chang, Y.-L.; Oey, L.-Y.
    Publisher: American Meteorological Society
    Abstract: ide gauge and satellite data reveal an interannual oscillation of the ocean?s thermoclines east of the Philippines and Taiwan, forced by a corresponding oscillation in the wind stress curl. This so-called Philippines?Taiwan ...
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    Deep Eddy Energy and Topographic Rossby Waves in the Gulf of Mexico 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 012:;page 3499
    Author(s): Oey, L-Y.; Lee, H-C.
    Publisher: American Meteorological Society
    Abstract: Observations suggest the hypothesis that deep eddy kinetic energy (EKE) in the Gulf of Mexico can be accounted for by topographic Rossby waves (TRWs). It is presumed that the TRWs are forced by Loop Current (LC) pulsation, ...
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    Eddy and Wind-Forced Heat Transports in the Gulf of Mexico 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 012:;page 2728
    Author(s): Chang, Y-L.; Oey, L-Y.
    Publisher: American Meteorological Society
    Abstract: The Gulf of Mexico (GOM) receives heat from the Caribbean Sea via the Yucatan?Loop Current (LC) system, and the corresponding ocean heat content (OHC) is important to weather and climate of the continental United States. ...
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    Why Can Wind Delay the Shedding of Loop Current Eddies? 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 011:;page 2481
    Author(s): Chang, Y.-L.; Oey, L.-Y.
    Publisher: American Meteorological Society
    Abstract: It is first shown that wind in the Gulf of Mexico can delay the shedding of Loop Current eddies. A time-dependent, three-dimensional numerical experiment forced by a spatially and temporally constant westward wind stress ...
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    Loop Current Cycle: Coupled Response of the Loop Current with Deep Flows 

    Source: Journal of Physical Oceanography:;2010:;Volume( 041 ):;issue: 003:;page 458
    Author(s): Chang, Y.-L.; Oey, L.-Y.
    Publisher: American Meteorological Society
    Abstract: Although the upper-layer dynamics of the Loop Current and eddies in the Gulf of Mexico are well studied, the understanding of how they are coupled to the deep flows is limited. In this work, results from a numerical model ...
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