Articles | Volume 11, issue 3
https://doi.org/10.5194/cp-11-587-2015
https://doi.org/10.5194/cp-11-587-2015
Research article
 | 
27 Mar 2015
Research article |  | 27 Mar 2015

Late Weichselian and Holocene palaeoceanography of Storfjordrenna, southern Svalbard

M. Łącka, M. Zajączkowski, M. Forwick, and W. Szczuciński

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Short summary
Storfjordrenna was deglaciated about 13,950 cal yr BP. During the transition from the sub-glacial to glaciomarine setting, Arctic Waters dominated its hydrography. However, the waters were not uniformly cold and experienced several warmer spells. Atlantic Water began to flow onto the shelves off Svalbard and into Storfjorden during the early Holocene, leading to progressive warming and significant glacial melting. A surface-water cooling and freshening occurred in late Holocene.