| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6349999 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2014 | 73 Pages |
Abstract
Warmer than present conditions may have occurred due to northward warm water transport via the West Spitsbergen Current, but also the absence of sea-ice and consequent lower albedo could have played a role.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Kari Grøsfjeld, Stijn De Schepper, Karl Fabian, Katrine Husum, Soma Baranwal, Karin Andreassen, Jochen Knies,