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    Enhanced Wind-Driven Downwelling Flow in Warm Oceanic Eddy Features during the Intensification of Tropical Cyclone Isaac (2012): Observations and Theory 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 006:;page 1667
    Author(s): Jaimes, Benjamin; Shay, Lynn K.
    Publisher: American Meteorological Society
    Abstract: ropical cyclones (TCs) typically produce intense oceanic upwelling underneath the storm?s center and weaker and broader downwelling outside upwelled regions. However, several cases of predominantly downwelling responses ...
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    Mixed Layer Cooling in Mesoscale Oceanic Eddies during Hurricanes Katrina and Rita 

    Source: Monthly Weather Review:;2009:;volume( 137 ):;issue: 012:;page 4188
    Author(s): Jaimes, Benjamin; Shay, Lynn K.
    Publisher: American Meteorological Society
    Abstract: During favorable atmospheric conditions, Hurricanes Katrina and Rita deepened to category 5 over the Loop Current?s (LC) bulge associated with an amplifying warm core eddy. Both hurricanes subsequently weakened to category ...
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    Near-Inertial Wave Wake of Hurricanes Katrina and Rita over Mesoscale Oceanic Eddies 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 006:;page 1320
    Author(s): Jaimes, Benjamin; Shay, Lynn K.
    Publisher: American Meteorological Society
    Abstract: Tropical cyclones (TCs) Katrina and Rita moved as major hurricanes over energetic geostrophic ocean features in the Gulf of Mexico. Increased and reduced oceanic mixed layer (OML) cooling was measured following the passage ...
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    Loop Current Mixed Layer Energy Response to Hurricane Lili (2002). Part II: Idealized Numerical Simulations 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 006:;page 1173
    Author(s): Uhlhorn, Eric W.; Shay, Lynn K.
    Publisher: American Meteorological Society
    Abstract: n this second part of a two-part study, details of the upper-ocean response within an idealized baroclinic current to a translating tropical cyclone are examined in a series of nonlinear, reduced-gravity numerical simulations. ...
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    Loop Current Mixed Layer Energy Response to Hurricane Lili (2002). Part I: Observations 

    Source: Journal of Physical Oceanography:;2011:;Volume( 042 ):;issue: 003:;page 400
    Author(s): Uhlhorn, Eric W.; Shay, Lynn K.
    Publisher: American Meteorological Society
    Abstract: he ocean mixed layer response to a tropical cyclone within and immediately adjacent to the Gulf of Mexico Loop Current is examined. In the first of a two-part study, a comprehensive set of temperature, salinity, and current ...
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    Oceanic Heat Content Variability in the Eastern Pacific Ocean for Hurricane Intensity Forecasting 

    Source: Monthly Weather Review:;2010:;volume( 138 ):;issue: 006:;page 2110
    Author(s): Shay, Lynn K.; Brewster, Jodi K.
    Publisher: American Meteorological Society
    Abstract: Recent evidence supports the premise that the subsurface ocean structure plays an important role in modulating air?sea fluxes during hurricane passage, which in turn, affects intensity change. Given the generally sparse ...
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    Loop Current Response to Hurricanes Isidore and Lili 

    Source: Monthly Weather Review:;2008:;volume( 136 ):;issue: 009:;page 3248
    Author(s): Shay, Lynn K.; Uhlhorn, Eric W.
    Publisher: American Meteorological Society
    Abstract: Recent hurricane activity over the Gulf of Mexico basin has underscored the importance of the Loop Current (LC) and its deep, warm thermal structure on hurricane intensity. During Hurricanes Isidore and Lili in 2002, ...
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    Free Surface Effects on the Near-Inertial Ocean Current Response to a Hurricane: A Revisit 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 001:;page 23
    Author(s): Shay, Lynn K.; Chang, Simon W.
    Publisher: American Meteorological Society
    Abstract: Free surface effects induced by an idealized hurricane based on observed air?sea variables in Hurricane Frederic are revisited to examine the barotropic and baroclinic response. Over five inertial periods comparisons between ...
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    Near-Inertial Ocean Current Response to Hurricane Frederic 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 008:;page 1249
    Author(s): Shay, Lynn K.; Elsberry, Russell L.
    Publisher: American Meteorological Society
    Abstract: Hurricane Frederic passed with 80 to 130 km of the U.S. Naval Oceanographic Office current meter arrays in water depths ranging from 100 to 470 m near the DeSoto Canyon region, and within 150 km of an Ocean Thermal Energy ...
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    The Role of Oceanic Mesoscale Features on the Tropical Cyclone–Induced Mixed Layer Response: A Case Study 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 004:;page 649
    Author(s): Jacob, S. Daniel; Shay, Lynn K.
    Publisher: American Meteorological Society
    Abstract: Oceanic mixed layer (ML) response to Hurricane Gilbert in the western Gulf of Mexico is investigated in this paper using the Miami Isopycnic Coordinate Ocean Model (MICOM). Three snapshots of oceanic observations indicated ...
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