Holocene sub-centennial evolution of Atlantic water inflow and sea ice distribution in the western Barents Sea

Holocene sub-centennial evolution of Atlantic water inflow and sea ice distribution in the western Barents Sea

A marine sediment core (JM09-KA11-GC) from the Kveithola Trough at the western Barents Sea margin has been investigated in order to reconstruct sub-surface temperatures and sea ice distribution at a sub-centennial resolution throughout the Holocene. The relationship between past variability of Atlan...

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Bibliographic Details
Main Authors: S. M. P. Berben, K. Husum, P. Cabedo-Sanz, S. T. Belt
Format: Article
Language:English
Published: Copernicus Publications 2014-01-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/10/181/2014/cp-10-181-2014.pdf

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