Icebergs in the North Atlantic: Modelling circulation changes and glaciomarine deposition.

Schäfer-Neth, C. and Stattegger, Karl (1999) Icebergs in the North Atlantic: Modelling circulation changes and glaciomarine deposition. In: Computerized Modeling of Sedimentary Systems. . Springer Berlin Heidelberg, Berlin Heidelberg, pp. 63-78. ISBN 978-3-642-08380-8 DOI 10.1007/978-3-662-03902-1_4.

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Abstract

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.

Document Type: Book chapter
Research affiliation: Kiel University
Publisher: Springer Berlin Heidelberg
Date Deposited: 30 Jan 2017 10:26
Last Modified: 30 Jan 2017 10:26
URI: https://oceanrep.geomar.de/id/eprint/35679

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