Svein Olaf Dahl
Svein Olaf Dahl
Professor in physical geography, Department of Geography, University of Bergen
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Holocene glacier fluctuations of Flatebreen and winter-precipitation changes in the Jostedalsbreen region, western Norvay, based on glaciolacustrine sediment records
A Nesje, JA Matthews, SO Dahl, MS Berrisford, C Andersson
The Holocene 11 (3), 267-280, 2001
A new approach to calculating Holocene winter precipitation by combining glacier equilibrium-line altitudes and pine-tree limits: a case stud from Hardangerjokulen, central …
SO Dahl, A Nesje
The Holocene 6 (4), 381-398, 1996
Norwegian mountain glaciers in the past, present and future
A Nesje, J Bakke, SO Dahl, Ø Lie, JA Matthews
Global and Planetary Change 60 (1-2), 10-27, 2008
Glaciers and Environmental Change
A Nesje, SO Dahl
Routledge, 2000
The ‘little ice age’–only temperature?
A Nesje, SO Dahl
The Holocene 13 (1), 139-145, 2003
Is the North Atlantic Oscillation reflected in Scandinavian glacier mass balance records?
A Nesje, Ø Lie, SO Dahl
Journal of Quaternary Science: Published for the Quaternary Research …, 2000
The Greenland 8200 cal. yr BP event detected in loss‐on‐ignition profiles in Norwegian lacustrine sediment sequences
A Nesje, SO Dahl
Journal of Quaternary Science: Published for the Quaternary Research …, 2001
Paleoclimatic implications based on equilibrium-line altitude depressions of reconstructed Younger Dryas and Holocene cirque glaciers in inner Nordfjord, western Norway
SO Dahl, A Nesje
Palaeogeography, Palaeoclimatology, Palaeoecology 94 (1-4), 87-97, 1992
Holocene glacier fluctuations at Hardangerjøkulen, central-southern Norway: a high-resolution composite chronology from lacustrine and terrestrial deposits
SO Dahl, A Nesje
The Holocene 4 (3), 269-277, 1994
Holocene glacier variations in central Jotunheimen, southern Norway based on distal glaciolacustrine sediment cores
JA Matthews, SO Dahl, A Nesje, MS Berrisford, C Andersson
Quaternary Science Reviews 19 (16), 1625-1647, 2000
The last ice sheet in north-west Scotland: reconstruction and implications
CK Ballantyne, D McCARROLL, A Nesje, SO Dahl, JO Stone
Quaternary Science Reviews 17 (12), 1149-1184, 1998
Glacier fluctuations, equilibrium-line altitudes and palaeoclimate in Lyngen, northern Norway, during the Lateglacial and Holocene
J Bakke, SO Dahl, Ø Paasche, R Løvlie, A Nesje
The Holocene 15 (4), 518-540, 2005
The lacustrine sedimentary sequence in Sygneskardvatnet, western Norway: a continuous, high-resolution record of the Jostedalsbreen ice cap during the Holocene
A Nesje, SO Dahl, C Andersson, JA Matthews
Quaternary Science Reviews 19 (11), 1047-1065, 2000
Utilizing physical sediment variability in glacier-fed lakes for continuous glacier reconstructions during the Holocene, northern Folgefonna, western Norway
J Bakke, Ø Lie, A Nesje, SO Dahl, Ø Paasche
The Holocene 15 (2), 161-176, 2005
Strength and spatial patterns of the Holocene wintertime westerlies in the NE Atlantic region
J Bakke, Ø Lie, SO Dahl, A Nesje, AE Bjune
Global and Planetary Change 60 (1-2), 28-41, 2008
Lateglacial and Holocene glacier fluctuations and climate variations in western Norway: a review
A Nesje, SO Dahl
Quaternary Science Reviews 12 (4), 255-261, 1993
Reconstruction of former glacier equilibrium-line altitudes based on proglacial sites: an evaluation of approaches and selection of sites
SO Dahl, J Bakke, Ø Lie, A Nesje
Quaternary Science Reviews 22 (2-4), 275-287, 2003
Timing, equilibrium-line altitudes and climatic implications of two early-Holocene glacier readvances during the Erdalen Event at Jostedalsbreen, western Norway
SO Dahl, A Nesje, Ø Lie, K Fjordheim, JA Matthews
The Holocene 12 (1), 17-25, 2002
Automated classification of debris-covered glaciers combining optical, SAR and topographic data in an object-based environment
BA Robson, C Nuth, SO Dahl, D Hölbling, T Strozzi, PR Nielsen
Remote Sensing of Environment 170, 372-387, 2015
Late Holocene surface ocean conditions of the Norwegian Sea (Vøring Plateau)
C Andersson, B Risebrobakken, E Jansen, SO Dahl
Paleoceanography 18 (2), 2003
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