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    Climate Drift in a Multicentury Integration of the NCAR Climate System Model 

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 006:;page 1455
    Author(s): Bryan, Frank O.
    Publisher: American Meteorological Society
    Abstract: The National Center for Atmospheric Research?s Climate System Model is a comprehensive model of the physical climate system. A 300-yr integration of the model has been carried out without flux correction. The solution shows ...
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    A Comparison of Mesoscale Eddy Heat Fluxes from Observations and a High-Resolution Ocean Model Simulation of the Kuroshio Extension 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 012:;page 2563
    Author(s): Bishop, Stuart P.; Bryan, Frank O.
    Publisher: American Meteorological Society
    Abstract: or the first time estimates of divergent eddy heat flux (DEHF) from a high-resolution (0.1°) simulation of the Parallel Ocean Program (POP) are compared with estimates made during the Kuroshio Extension System Study (KESS). ...
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    Bjerknes-like Compensation in the Wintertime North Pacific 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 005:;page 1339
    Author(s): Bishop, Stuart P.; Bryan, Frank O.; Small, R. Justin
    Publisher: American Meteorological Society
    Abstract: bservational and model evidence has been mounting that mesoscale eddies play an important role in air?sea interaction in the vicinity of western boundary currents and can affect the jet stream storm track. What is less ...
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    Surface Ocean Fluxes and Water-Mass Transformation Rates in the Coupled NCAR Climate System Model 

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 006:;page 1420
    Author(s): Doney, Scott C.; Large, William G.; Bryan, Frank O.
    Publisher: American Meteorological Society
    Abstract: The global distributions of the air?sea fluxes of heat and freshwater and water mass transformation rates from a control integration of the coupled National Center for Atmospheric Research (NCAR) Climate System Model (CSM) ...
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    Application of a Third-Order Upwind Scheme in the NCAR Ocean Model 

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 006:;page 1487
    Author(s): Holland, William R.; Chow, Julianna C.; Bryan, Frank O.
    Publisher: American Meteorological Society
    Abstract: The National Center for Atmospheric Research (NCAR) Ocean Model has been developed for use in NCAR?s Climate System Modeling project, a comprehensive development of a coupled ocean?atmosphere?sea ice?land surface model of ...
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    Can Southern Ocean Eddy Effects Be Parameterized in Climate Models? 

    Source: Journal of Climate:;2013:;volume( 027 ):;issue: 001:;page 411
    Author(s): Bryan, Frank O.; Gent, Peter R.; Tomas, Robert
    Publisher: American Meteorological Society
    Abstract: resent-day control and 1% yr?1 increasing carbon dioxide runs have been made using two versions of the Community Climate System Model, version 3.5. One uses the standard versions of the ocean and sea ice components where ...
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    On the Midlatitude Circulation in a High-Resolution Model of the North Atlantic 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 003:;page 289
    Author(s): Bryan, Frank O.; Böning, Claus W.; Holland, William R.
    Publisher: American Meteorological Society
    Abstract: This paper describes, and establishes the dynamical mechanisms responsible for, the large-scale, time-mean, midlatitude circulation in a high-resolution model of the North Atlantic basin. The model solution is compared ...
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    On the Seasonal Cycle of the Tropical South Indian Ocean. Part I: Mixed Layer Heat and Salt Budgets 

    Source: Journal of Climate:;2019:;volume 032:;issue 006:;page 1951
    Author(s): Soares, Saulo M.; Richards, Kelvin J.; Bryan, Frank O.; Yoneyama, Kunio
    Publisher: American Meteorological Society
    Abstract: AbstractScale interactions in the coupled ocean and atmosphere of the tropics play a crucial role in shaping the climate state and its spatial and temporal variability. The mechanisms driving the seasonal cycles of mixed ...
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    Air–Sea Turbulent Heat Fluxes in Climate Models and Observational Analyses: What Drives Their Variability? 

    Source: Journal of Climate:;2019:;volume 032:;issue 008:;page 2397
    Author(s): Small, R. Justin; Bryan, Frank O.; Bishop, Stuart P.; Tomas, Robert A.
    Publisher: American Meteorological Society
    Abstract: AbstractA traditional view is that the ocean outside of the tropics responds passively to atmosphere forcing, which implies that air?sea heat fluxes are mainly driven by atmosphere variability. This paper tests this viewpoint ...
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    Climatological Annual Cycle of the Salinity Budgets of the Subtropical Maxima 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 010:;page 2981
    Author(s): Johnson, Benjamin K.; Bryan, Frank O.; Grodsky, Semyon A.; Carton, James A.
    Publisher: American Meteorological Society
    Abstract: ix subtropical salinity maxima (Smax) exist: two each in the Pacific, Atlantic, and Indian Ocean basins. The north Indian (NI) Smax lies in the Arabian Sea while the remaining five lie in the open ocean. The annual cycle ...
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