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    A Global Analysis of Sverdrup Balance Using Absolute Geostrophic Velocities from Argo 

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 004:;page 1213
    Author(s): Gray, Alison R.; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: sing observations from the Argo array of profiling floats, the large-scale circulation of the upper 2000 decibars (db) of the global ocean is computed for the period from December 2004 to November 2010. The geostrophic ...
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    A Nonconservative β-Spiral Determination of the Deep Circulation in the Eastern South Pacific 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 009:;page 1975
    Author(s): Hautala, Susan L.; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: The horizontal mean circulation and diapycnal flux divergence field in the South Pacific between Tahiti and the East Pacific Rise are obtained from a nonconservative ?-spiral inverse method applied to high quality hydrographic ...
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    An Assessment of the Seasonal Salinity Budget for the Upper Bay of Bengal 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 005:;page 1361
    Author(s): Wilson, Earle A.; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: uring each summer monsoon, the Bay of Bengal is inundated by a large amount of rain and river discharge. The effects of this freshening are gradually reversed over the course of the year, with near-surface salinities ...
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    Reply to “Comments on ‘A Global Analysis of Sverdrup Balance Using Absolute Geostrophic Velocities from Argo’” 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 005:;page 1449
    Author(s): Gray, Alison R.; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: his response addresses the three comments by A. Polonsky on ?A Global Analysis of Sverdrup Balance Using Absolute Geostrophic Velocities from Argo.?
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    RAFOS Floats: Defining and Targeting Surfaces of Neutral Buoyancy 

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 004:;page 1079
    Author(s): Swift, Dana D.; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: For timescales much greater than the local buoyancy period, the buoyant response of a RAFOS float is virtually dictated by its compressibility. As the compressibility of a thermally inert RAFOS float increases from zero, ...
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    Idealized Models of Slantwise Convection in a Baroclinic Flow 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 002:;page 558
    Author(s): Straneo, Fiammetta; Kawase, Mitsuhiro; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: Intermediate, or deep, convection in a baroclinic flow occurs along slanted paths parallel to the alongflow absolute momentum surfaces. These surfaces are principally tilted due to the vertical shear in velocity but can ...
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    Potential Vorticity Dynamics of Boundary Currents in a Quasi-geostrophic Ocean 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 009:;page 1373
    Author(s): Lozier, M. Susan; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: Boundary layer potential vorticity dynamics for a quasi-geostrophic, eddy-resolving general circulation ocean model are studied using both Lagrangian and Eulerian analyses. Active western boundary layers are found not only ...
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    A Simple Model of Abyssal Circulation, Including Effects of Wind, Buoyancy and Topography 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 005:;page 596
    Author(s): Hautala, Susan L.; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: We examine problems of steady abyssal circulation using an inviscid planetary geostrophic layered model. The model includes an active wind-driven upper layer and arbitrary topography; forcing is in the form of specified ...
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    Potential Vorticity Sources and Sinks in a Quasi-geostrophic Ocean: beyond Western Boundary Currents 

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 010:;page 1608
    Author(s): Lozier, M. Susan; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: Potential vorticity dynamics for a quasi-geostrophic eddy-resolving general circulation model (EGCM) are studied in order to determine the effects of mesoscale variability on the potential vorticity distribution of a ...
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    Profiling Float Observations of the Upper Ocean under Sea Ice off the Wilkes Land Coast of Antarctica 

    Source: Journal of Physical Oceanography:;2011:;Volume( 041 ):;issue: 006:;page 1102
    Author(s): Wong, Annie P. S.; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: ultiyear under-ice temperature and salinity data collected by profiling floats are used to study the upper ocean near the Wilkes Land coast of Antarctica. The study region is in the seasonal sea ice zone near the southern ...
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    DSpace software copyright © 2002-2015  DuraSpace
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