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Bjørg Risebrobakken, Trond Dokken, Lars Henrik Smedsrud, Carin Andersson, Eystein Jansen, Matthias Moros and Elena V. Ivanova Early Holocene temperature variability in the Nordic Seas: The role of oceanic heat advection versus changes in orbital forcing Paleoceanography 26

Article first published online: 22 OCT 2011 | DOI: 10.1029/2011PA002117

Key Points

  • Maximum northward heat advection to the Nordic Seas at 10 ka BP
  • Insolation driven thermal maximum 9–6 ka, only seen in the summer mixed layer
  • Strong influence of meltwater, gradually diminishing, 12–8.5 ka

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