Articles | Volume 6, issue 6
Clim. Past, 6, 817–826, 2010
Clim. Past, 6, 817–826, 2010

Research article 20 Dec 2010

Research article | 20 Dec 2010

Warm Nordic Seas delayed glacial inception in Scandinavia

A. Born1,2,3,*, M. Kageyama3, and K. H. Nisancioglu1,4 A. Born et al.
  • 1Bjerknes Centre for Climate Research, Bergen, Norway
  • 2Geophysical Institute, University of Bergen, Bergen, Norway
  • 3Laboratoire des Sciences du Climat et l'Environnement, Gif sur Yvette, France
  • 4UNI Research, Bergen, Norway
  • *now at: Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland

Abstract. We simulate the last glacial inception, 115 000 years ago, with a three dimensional thermomechanical ice sheet model of the Northern Hemisphere, forced by a comprehensive coupled climate model. High oceanic heat transport into the Nordic Seas prevents large scale ice growth over Scandinavia. Glacial inception in the region starts on the highest mountains in the south when sea surface temperatures in the Nordic Seas are reduced by at least 3 °C. Ice growth in Northern Scandinavia requires a cooling by at least 4 °C. This is in good agreement with marine proxy data from the Nordic Seas and North Atlantic as well as available terrestrial data. This study thus provides a physical understanding and revised timing of the first glacier advance over Scandinavia.