J
Jan Sverre Laberg
Researcher at University of Tromsø
Publications - 138
Citations - 6712
Jan Sverre Laberg is an academic researcher from University of Tromsø. The author has contributed to research in topics: Continental margin & Continental shelf. The author has an hindex of 44, co-authored 128 publications receiving 6140 citations.
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Morphology of Younger Dryas subglacial and ice-proximal submarine landforms, inner Vestfjorden, northern Norway
TL;DR: In this article, the sea floor morphology of two pronounced across-fjord bedrock thresholds located at the mouths of Ofotføorden and Tysføjorden, northern Norway, has been analyzed based on swath bathymetry and seismic data.
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Pleistocene depositional environments and links to cryosphere-ocean interactions on the eastern Ross Sea continental slope, Antarctica (IODP Hole U1525A)
Maxine V. King,J. A. Gales,Jan Sverre Laberg,Robert M. McKay,Laura De Santis,Denise K. Kulhanek,Phil Hosegood,Antony Morris,Iodp Expedition Scientists +8 more
TL;DR: In this article, the authors investigate the upper 121m of Hole U1525A, collected during International Ocean Discovery Program (IODP) Expedition 374 in 2018, and develop a lithofacies scheme that allows construction of a detailed depositional model and environmental history of past ice sheet-ocean interactions at the eastern Ross Sea continental shelf break/slope since 2.4.
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Geomorphology and development of a high-latitude channel system: the INBIS channel case (NW Barents Sea, Arctic)
L. Rui,Michele Rebesco,J. L. Casamor,Jan Sverre Laberg,Tom Arne Rydningen,Andrea Caburlotto,Matthias Forwick,Roger Urgeles,Daniela Accettella,Renata G. Lucchi,Ivana Delbono,M. Barsanti,Maurizio Demarte,Roberta Ivaldi +13 more
TL;DR: In this article, a post-peer review, pre-copyedit version of an article published in Arktos is presented, with a pre-copedit version available online at https://doi.org/10.1007/s41063-019-00065-9.
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Eskers in deglacial sediments of three Spitsbergen fjords
TL;DR: Benn et al. as discussed by the authors distinguished four basic esker types: tunnel fills, formed in englacial and subglacial conduits and exposed by ice ablation; ice-channel fills, deposited in sub-aerial, ice-walled channels; segmented tunnel fills during stepwise glacier retreat; and beaded eskers, composed of subaqueous fans.
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Corrigendum to “Deglaciation of a marine-based ice sheet: Late Weichselian palaeo-ice dynamics and retreat in the southern Barents Sea reconstructed from onshore and offshore glacial geomorphology” [Quat. Sci. Rev. 29 (2010) 424-442]
TL;DR: In this paper, a marine-based ice sheet is reconstructed from onshore and offshore glacial geomorphology from the southern Barents Sea using the late Weichselian palaeo-ice dynamics and retreat.