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    Isopycnal and Diapycnal Mixing at the Cape Verde Frontal Zone 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 008:;page 1771
    Author(s): Klein, Birgit; Siedler, Gerold
    Publisher: American Meteorological Society
    Abstract: The Cape Verde Frontal Zone separates the North and the South Atlantic Central Waters in the eastern North Atlantic. It also represents the boundary between the ventilated subtropical gyre and the quasi-stagnant shadow ...
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    The Meridional Oceanic Transports of Heat and Nutrients in the South Atlantic 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 001:;page 5
    Author(s): Holfort, Jürgen; Siedler, Gerold
    Publisher: American Meteorological Society
    Abstract: Meridional transports of mass, heat, nutrients, and carbon across coast-to-coast WOCE and pre-WOCE sections between 11°S and 45°S in the South Atlantic are calculated using an inverse model. Usually salt preservation is ...
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    The Volunteer Observing Ship and Future Ocean Monitoring 

    Source: Bulletin of the American Meteorological Society:;1995:;volume( 076 ):;issue: 001:;page 5
    Author(s): Rossby, Thomas; Siedler, Gerold; Zenk, Walter
    Publisher: American Meteorological Society
    Abstract: Widespread and sustained in situ ocean measurements are essential to an improved understanding of the state of the ocean and its role in global change. Merchant marine vessels can play a major role in ocean monitoring, yet ...
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    The Madeira Mode Water 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 010:;page 1561
    Author(s): Siedler, Gerold; Kuhl, Anni; Zenk, Walter
    Publisher: American Meteorological Society
    Abstract: Quasi-homogeneous layers in vertical profiles of temperature and salinity in the eastern North Atlantic near Madeira indicate the existence of a subtropical Mode Water in the Eastern Basin. Temperature sections show a ...
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    Dynamics of Intermediate Water Circulation in the Subtropical South Atlantic 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 012:;page 3191
    Author(s): Schmid, Claudia; Siedler, Gerold; Zenk, Walter
    Publisher: American Meteorological Society
    Abstract: The circulation of the low-salinity Antarctic Intermediate Water in the South Atlantic and the associated dynamical processes are studied, using recent and historical hydrographic profiles, Lagrangian and Eulerian current ...
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    Circulation and Variability at the Southern Boundary of the Brazil Basin 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 002:;page 145
    Author(s): Hogg, Nelson G.; Siedler, Gerold; Zenk, Walter
    Publisher: American Meteorological Society
    Abstract: As a contribution to the WOCE Deep Basin Experiment, an array of current meters with individual record lengths exceeding 1½ years was set across the southern boundary of the Brazil Basin between early 1991 and early 1996. ...
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    Antarctic Bottom Water Flow through the Hunter Channel 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 011:;page 2785
    Author(s): Zenk, Walter; Siedler, Gerold; Lenz, Bernd; Hogg, Nelson G.
    Publisher: American Meteorological Society
    Abstract: The Rio Grande Rise acts as a natural barrier for the equatorward flow of Antarctic Bottom Water in the subtropical South Atlantic. In addition to the Vema Channel, the Hunter Channel cuts through this obstacle and offers ...
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    Baroclinic Flow and Transient-Tracer Fields in the Canary–Cape Verde Basin 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 005:;page 814
    Author(s): Thiele, Gerhard; Roether, Wolfgang; Schlosser, Peter; Kuntz, Reinhard; Siedler, Gerold; Stramma, Lothar
    Publisher: American Meteorological Society
    Abstract: Simulated transient-tracer distributions (tritium, 3H3, freons) on the isopycnal horizons σ0=26.5 and 26.8 kg m?3 are presented for the East Atlantic, 10° ?40°N. Tracer transport is modeled by employing a baroclinic flow ...
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    Deep-Water Flow in the Mariana and Caroline Basins 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 003:;page 566
    Author(s): Siedler, Gerold; Holfort, Jürgen; Zenk, Walter; Müller, Thomas J.; Csernok, Tiberiu
    Publisher: American Meteorological Society
    Abstract: Two major water masses dominate the deep layers in the Mariana and Caroline Basins: the Lower Circumpolar Water (LCPW), arriving from the Southern Ocean along the slopes north of the Marshall Islands, and the North Pacific ...
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