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    An Equatorial Diffusive Boundary Layer and the Equatorial Stacked Jets in Thermally Driven OGCMs 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 009:;page 2737
    Author(s): Furue, Ryo
    Publisher: American Meteorological Society
    Abstract: New equatorial boundary layer solutions are found in a reduced-gravity model with large horizontal diffusivity. Analytical and semianalytical solutions are obtained and the structure of the boundary layer is discussed. The ...
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    Energy Transfer within the Small-Scale Oceanic Internal Wave Spectrum 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 001:;page 267
    Author(s): Furue, Ryo
    Publisher: American Meteorological Society
    Abstract: Three-dimensional numerical experiments are conducted to examine energy transfer within the small-scale portion of the Garrett?Munk model spectrum of oceanic internal waves. The rate of energy transfer in the experiments ...
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    Effects of the Pacific Diapycnal Mixing and Wind Stress on the Global and Pacific Meridional Overturning Circulation 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 010:;page 1876
    Author(s): Furue, Ryo; Endoh, Masahiro
    Publisher: American Meteorological Society
    Abstract: Numerical experiments are conducted using an idealized basin to investigate roles of the deep vertical diffusivity and wind stress of the Pacific Ocean in the global and Pacific meridional overturning circulation. The ...
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    Dynamics of the Northern Tsuchiya Jet 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 009:;page 2024
    Author(s): Furue, Ryo; McCreary, Julian P.; Yu, Zuojun
    Publisher: American Meteorological Society
    Abstract: The Tsuchiya jets (TJs) are narrow eastward currents located along thermal fronts at the poleward edges of thermostad water in the Pacific Ocean. In this study, an oceanic general circulation model (OGCM) is used to explore ...
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    The South China Sea Throughflow Retrieved from Climatological Data 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 003:;page 753
    Author(s): Yaremchuk, Max; McCreary, Julian; Yu, Zuojun; Furue, Ryo
    Publisher: American Meteorological Society
    Abstract: The salinity distribution in the South China Sea (SCS) has a pronounced subsurface maximum from 150?220 m throughout the year. This feature can only be maintained by the existence of a mean flow through the SCS, consisting ...
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    Influence of Eddy Momentum Fluxes on the Mean Flow of the Kuroshio Extension in a 1/10° Ocean General Circulation Model 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 009:;page 2769
    Author(s): Aoki, Kunihiro; Kubokawa, Atsushi; Furue, Ryo; Sasaki, Hideharu
    Publisher: American Meteorological Society
    Abstract: his study explores the role of the momentum flux divergence due to mesoscale eddies for the maintenance of the Kuroshio Extension (KE) jet. For that purpose, the zonal momentum budget in a high-resolution ocean general ...
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    Comparison of Two Classical Advection Schemes in a General Circulation Model 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 009:;page 2439
    Author(s): Yamanaka, Yasuhiro; Furue, Ryo; Hasumi, Hiroyasu; Suginohara, Nobuo
    Publisher: American Meteorological Society
    Abstract: The authors compare two classical advection schemes, the centered difference and weighted upcurrent, for coarse-resolution OGCMs, using an idealized ocean basin and a realistic World Ocean topography. For the idealized ...
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    Dynamics of the Southern Tsuchiya Jet 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 003:;page 531
    Author(s): Furue, Ryo; McCreary, Julian P.; Yu, Zuojun; Wang, Dailin
    Publisher: American Meteorological Society
    Abstract: The Tsuchiya jets (TJs) are narrow eastward currents, located a few degrees on either side of the equator at depths from 200 to 500 m in the Pacific Ocean. In this study, non-eddy-resolving, oceanic general circulation ...
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    Subsurface Salinity Balance in the South China Sea 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 002:;page 527
    Author(s): Yu, Zuojun; McCreary, Julian P.; Yaremchuk, Max; Furue, Ryo
    Publisher: American Meteorological Society
    Abstract: The South China Sea (SCS) is often treated as a semienclosed water body, with the Luzon Strait as its only connection to the Pacific Ocean. A branch of the Kuroshio flows northwestward across the Luzon Strait to enter the ...
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    Dynamics of a Quasi-Stationary Jet along the Subarctic Front in the North Pacific Ocean (the Western Isoguchi Jet): An Ideal Two-Layer Model 

    Source: Journal of Physical Oceanography:;2018:;volume 048:;issue 004:;page 807
    Author(s): Miyama, Toru; Mitsudera, Humio; Nishigaki, Hajime; Furue, Ryo
    Publisher: American Meteorological Society
    Abstract: ABSTRACTThe dynamics of a quasi-stationary jet along the Subarctic Front in the North Pacific Ocean (the Western Isoguchi Jet) were investigated using an idealized two-layer model. The experiments suggested that a seafloor ...
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