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    The Flow of Antarctic Bottom Water into the Brazil Basin 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 012:;page 2667
    Author(s): Speer, Kevin G.; Zenk, Walter
    Publisher: American Meteorological Society
    Abstract: The total transport of Antarctic Bottom Water across the Rio Grande Rise, including the western boundary, the Vema Channel, and the Hunter Channel is estimated from hydrographic measurements across these pathways. The ...
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    Transport of Bottom Water in the Romanche Fracture Zone and the Chain Fracture Zone 

    Source: Journal of Physical Oceanography:;1998:;Volume( 028 ):;issue: 005:;page 779
    Author(s): Mercier, Herlé; Speer, Kevin G.
    Publisher: American Meteorological Society
    Abstract: Two moored arrays deployed in the Romanche Fracture Zone and Chain Fracture Zone in the equatorial Atlantic Ocean provide two-year-long time series of current and temperature in the Lower North Atlantic Deep Water and the ...
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    Bottom Water Circulation in the Western North Atlantic 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 001:;page 83
    Author(s): Speer, Kevin G.; McCartney, Michael S.
    Publisher: American Meteorological Society
    Abstract: Antarctic Bottom Water flows into the western North Atlantic across the equator, shifting from the western side to the eastern side of the trough between the American continents and the Mid-Atlantic Ridge as it continues ...
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    Multiple Zonal Jets in a Differentially Heated Rotating Annulus 

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 009:;page 2273
    Author(s): Smith, Carlowen A.; Speer, Kevin G.; Griffiths, Ross W.
    Publisher: American Meteorological Society
    Abstract: laboratory experiment of multiple baroclinic zonal jets is described, thought to be dynamically similar to flow observed in the Antarctic Circumpolar Current. Differential heating sets the overall temperature difference ...
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    Water Mass Formation from Revised COADS Data 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 010:;page 2444
    Author(s): Speer, Kevin G.; Isemer, H-J.; Biastoch, A.
    Publisher: American Meteorological Society
    Abstract: Surface heat and freshwater fluxes from the Comprehensive 0cean-Atmosphere Data Set are revised and used diagnostically to compute air-sea transformation rates on density, temperature, and salinity classes over the domain ...
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    Gyres and Jets: Inversion of Tracer Data for Ocean Circulation Structure 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 006:;page 1180
    Author(s): Herbei, Radu; McKeague, Ian W.; Speer, Kevin G.
    Publisher: American Meteorological Society
    Abstract: This paper describes a quasi-3D Bayesian inversion of oceanographic tracer data from the South Atlantic Ocean. Initially, one active neutral-density layer is considered with an upper and lower boundary. The available ...
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    Transport across 48°N in the Atlantic Ocean 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 004:;page 733
    Author(s): Lumpkin, Rick; Speer, Kevin G.; Koltermann, K. Peter
    Publisher: American Meteorological Society
    Abstract: Transports across 48°N in the Atlantic Ocean are estimated from five repeat World Ocean Circulation Experiment (WOCE) hydrographic lines collected in this region in 1993?2000, from time-varying air?sea heat and freshwater ...
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    Tracing Southwest Pacific Bottom Water Using Potential Vorticity and Helium-3 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 012:;page 2153
    Author(s): Downes, Stephanie M.; Key, Robert M.; Orsi, Alejandro H.; Speer, Kevin G.; Swift, James H.
    Publisher: American Meteorological Society
    Abstract: his study uses potential vorticity and other tracers to identify the pathways of the densest form of Circumpolar Deep Water in the South Pacific, termed ?Southwest Pacific Bottom Water? (SPBW), along the 28.2 kg m?3 surface. ...
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    Circulation and Stirring in the Southeast Pacific Ocean and the Scotia Sea Sectors of the Antarctic Circumpolar Current 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 007:;page 2005
    Author(s): Balwada, Dhruv; Speer, Kevin G.; LaCasce, Joseph H.; Owens, W. Brechner; Marshall, John; Ferrari, Raffaele
    Publisher: American Meteorological Society
    Abstract: he large-scale middepth circulation and eddy diffusivities in the southeast Pacific Ocean and Scotia Sea sectors between 110° and 45°W of the Antarctic Circumpolar Current (ACC) are described based on a subsurface ...
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    Does the Potential Vorticity Distribution Constrain the Spreading of Floats in the North Atlantic? 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 004:;page 721
    Author(s): O’Dwyer, Jane; Williams, Richard G.; LaCasce, Joseph H.; Speer, Kevin G.
    Publisher: American Meteorological Society
    Abstract: Float trajectories are compared with the distribution of climatological potential vorticity, Q, on approximate isentropic surfaces for intermediate waters in the North Atlantic. The time-mean displacement and eddy dispersion ...
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