Now showing items 1-2 of 2

    • Greenland-Scotland overflow studied by hydro-chemical multivariate analysis 

      Fogelquist, E.; Blindheim, J.; Tanhua, Toste; Østerhus, Svein; Buch, E.; Rey, Francisco (Elsevier, 2003-01)
      Hydrographic, nutrient and halocarbon tracer data collected in July-August 1994 in the Norwegian Sea, the Faroe Bank Channel (FBC), the Iceland and Irminger Basins and the Iceland Sea are resented. Special attention was ...
      Journal articlePeer reviewed
    • Intermediate water from the Greenland Sea in the Faroe Bank Channel : spreading of released sulphur hexafluoride 

      Olsson, K. Anders; Jeansson, Emil; Anderson, Leif G.; Hansen, Bogi; Eldevik, Tor; Kristiansen, Regin; Messias, Marie-José; Johannessen, Truls; Watson, Andrew J. (Elsevier, 2005-02)
      The Faroe Bank Channel is the deepest passage for dense water leaving the Nordic Seas into the North Atlantic. The contribution to this part of the Greenland-Scotland Overflow by intermediate water from the Greenland ...
      Journal article