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    Is Bottom Boundary Layer Mixing Slowly Ventilating Greenland Sea Deep Water 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 001:;page 215
    Author(s): Visbeck, Martin; Rhein, Monika
    Publisher: American Meteorological Society
    Abstract: Bottom water temperatures in the central Greenland Sea have been increasing for the last two decades. The warming is most likely related to the absence of deep convective mixing, which cools and freshens the deep water. ...
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    Variability of the Overflow Water Transport in the Western Subpolar North Atlantic, 1950–97 

    Source: Journal of Physical Oceanography:;2006:;Volume( 036 ):;issue: 003:;page 435
    Author(s): Kieke, Dagmar; Rhein, Monika
    Publisher: American Meteorological Society
    Abstract: One of the major topics in current field research is the question of whether or to what extent the North Atlantic Ocean is subject to changes in water mass transports, and how they are related to atmospheric phenomena like ...
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    Variability in the Internal Wave Field Induced by the Atlantic Deep Western Boundary Current at 16°N 

    Source: Journal of Physical Oceanography:;2013:;Volume( 044 ):;issue: 002:;page 492
    Author(s): Köhler, Janna; Mertens, Christian; Walter, Maren; Stöber, Uwe; Rhein, Monika; Kanzow, Torsten
    Publisher: American Meteorological Society
    Abstract: ive years of continuous mooring data combined with conductivity?temperature?depth (CTD)/lowered acoustic Doppler current profiler (LADCP) measurements from five cruises are used to investigate the influence of the deep ...
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    Changes in the CFC Inventories and Formation Rates of Upper Labrador Sea Water, 1997–2001 

    Source: Journal of Physical Oceanography:;2006:;Volume( 036 ):;issue: 001:;page 64
    Author(s): Kieke, Dagmar; Rhein, Monika; Stramma, Lothar; Smethie, William M.; LeBel, Deborah A.; Zenk, Walter
    Publisher: American Meteorological Society
    Abstract: Chlorofluorocarbon (component CFC-11) and hydrographic data from 1997, 1999, and 2001 are presented to track the large-scale spreading of the Upper Labrador Sea Water (ULSW) in the subpolar gyre of the North Atlantic Ocean. ...
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