Icebergs in the North Atlantic: Modelling Circulation Changes and Glacio-Marine Deposition

  • C. Schäfer-Neth
  • K. Stattegger
Conference paper


Meltwater events (MWE) during and at the end of the last glaciation led to dramatic changes in the oceanic circulation of the North Atlantic combined with a strong reduction in deepwater formation or even a breakdown of the conveyor belt (Bond 1995; Bond and Lotti 1995; Broecker 1991; Seidov et al. 1996). These changes depend on (i) the amount of freshwater brought in and (ii) the locations of freshwater input and its transport path; that means the conditions to form one or several large freshwater lenses on top of the water column in the central Greenland, Iceland, and Norwegian (GIN) Seas.


Last Glacial Maximum Heinrich Event Modular Ocean Model East Greenland Current Oxygen Isotope Measurement 
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© Springer-Verlag Berlin Heidelberg 1999

Authors and Affiliations

  • C. Schäfer-Neth
  • K. Stattegger

There are no affiliations available

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