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    The Sensitivity of the Arctic Ocean Sea Ice Thickness and Its Dependence on the Surface Albedo Parameterization 

    Source: Journal of Climate:;2012:;volume( 026 ):;issue: 004:;page 1355
    Author(s): Björk, Göran; Stranne, Christian; Borenäs, Karin
    Publisher: American Meteorological Society
    Abstract: n this study, the response of sea ice thickness to changes in the external forcing is investigated and particularly how this response depends on the surface albedo formulation by means of a one-dimensional coupled ...
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    Potential-Vorticity Characteristics of the Faroe Bank Channel Deep-Water Overflow 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 006:;page 921
    Author(s): Lake, Iréne; Borenäs, Karin; Lundberg, Peter
    Publisher: American Meteorological Society
    Abstract: Results from a 71-day deployment of three ADCP current meters on a section across the sill region of the Faroe Bank Channel are reported. The characteristic density structure of the channel, with warm, highly saline North ...
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    Comments on “Is the Faroe Bank Channel Overflow Hydraulically Controlled?” 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 006:;page 1534
    Author(s): Enmar, Linda; Borenäs, Karin; Lake, Iréne; Lundberg, Peter
    Publisher: American Meteorological Society
    Abstract: In a recent paper Girton et al., due to what appears to be a misunderstanding, stated that a critical-flow analysis of the deep-water transport through the Faroe Bank Channel had been undertaken by Lake et al. on the basis ...
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    On the Intermediate Water Masses of the Faroe–Bank Channel Overflow 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 007:;page 1904
    Author(s): Borenäs, Karin M.; Lake, Irène L.; Lundberg, Peter A.
    Publisher: American Meteorological Society
    Abstract: A review of available hydrographic data from the Faroe?Bank Channel indicates that North Icelandic/Arctic Intermediate water masses are present in the passage to a larger extent than was previously believed. The presently ...
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