Articles | Volume 9, issue 5
https://doi.org/10.5194/cp-9-2365-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-9-2365-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Pre-LGM Northern Hemisphere ice sheet topography
J. Kleman
Department of Physical Geography and Quaternary Geology, Stockholm University, Bolin Centre for Climate Research, 10691, Stockholm, Sweden
J. Fastook
Department of Computer Science, University of Maine, Orono, ME 04469-5790, USA
Department of Physical Geography and Quaternary Geology, Stockholm University, Bolin Centre for Climate Research, 10691, Stockholm, Sweden
J. Nilsson
Department of Meteorology, Stockholm University, Bolin Centre for Climate Research, 10691, Stockholm, Sweden
R. Caballero
Department of Meteorology, Stockholm University, Bolin Centre for Climate Research, 10691, Stockholm, Sweden
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The Cryosphere, 10, 639–664, https://doi.org/10.5194/tc-10-639-2016, https://doi.org/10.5194/tc-10-639-2016, 2016
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We use a numerical model based on approximated ice flow physics and calibrated against field-based evidence to present numerical simulations of multiple advance and retreat phases of the former Cordilleran ice sheet in North America during the last glacial cycle (120 000 to 0 years before present).
M. Löfverström, R. Caballero, J. Nilsson, and J. Kleman
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Karin Ebert, Karin Ekstedt, and Jerker Jarsjö
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Future sea level rise is inevitable. We investigate the effects of 2 m sea level rise on the island of Gotland, Sweden. In a multi-criteria analysis we analyze the quantity of infrastructure that will be inundated, and the effect of saltwater intrusion in wells. Almost 100 km2 (3 %) of Gotland's land area will be inundated. Important touristic and nature values will be strongest affected. Well salinization will greatly increase. Administrative planning is needed to prepare for changes.
Julien Seguinot, Irina Rogozhina, Arjen P. Stroeven, Martin Margold, and Johan Kleman
The Cryosphere, 10, 639–664, https://doi.org/10.5194/tc-10-639-2016, https://doi.org/10.5194/tc-10-639-2016, 2016
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We use a numerical model based on approximated ice flow physics and calibrated against field-based evidence to present numerical simulations of multiple advance and retreat phases of the former Cordilleran ice sheet in North America during the last glacial cycle (120 000 to 0 years before present).
T. Hughes, A. Sargent, J. Fastook, K. Purdon, J. Li, J.-B. Yan, and S. Gogineni
The Cryosphere, 10, 193–225, https://doi.org/10.5194/tc-10-193-2016, https://doi.org/10.5194/tc-10-193-2016, 2016
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The Antarctic and Greenland ice sheets are drained primarily by fast ice streams that end as ice shelves if they become afloat. Smooth transitions from slow sheet flow to fast stream flow to confined shelf flow are obtained and applied to Byrd Glacier in Antarctica after two upstream subglacial lakes suddenly drained in 2006, and to Jakobshavn Isbrae in Greenland after a confined ice shelf suddenly disintegrated in 2002. Byrd Glacier quickly stabilized, but Jakobshavn Isbrae remains unstable.
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P. Schmidt, B. Lund, J-O. Näslund, and J. Fastook
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The Cryosphere Discuss., https://doi.org/10.5194/tcd-8-2043-2014, https://doi.org/10.5194/tcd-8-2043-2014, 2014
Revised manuscript not accepted
A. Sargent and J. L. Fastook
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Revised manuscript has not been submitted
Related subject area
Subject: Continental Surface Processes | Archive: Terrestrial Archives | Timescale: Pleistocene
Climate changes during the Late Glacial in southern Europe: new insights based on pollen and brGDGTs of Lake Matese in Italy
The climate and vegetation of Europe, North Africa and the Middle East during the Last Glacial Maximum (21,000 years BP) based on pollen data
Late Pleistocene glacial chronologies and paleoclimate in the northern Rocky Mountains
Cryogenic cave carbonates in the Dolomites (northern Italy): insights into Younger Dryas cooling and seasonal precipitation
Younger Dryas ice margin retreat in Greenland: new evidence from southwestern Greenland
Pleistocene glacial history of the New Zealand subantarctic islands
Palaeoclimate characteristics in interior Siberia of MIS 6–2: first insights from the Batagay permafrost mega-thaw slump in the Yana Highlands
Hydroclimate of the Last Glacial Maximum and deglaciation in southern Australia's arid margin interpreted from speleothem records (23–15 ka)
High-amplitude lake-level changes in tectonically active Lake Issyk-Kul (Kyrgyzstan) revealed by high-resolution seismic reflection data
Constant wind regimes during the Last Glacial Maximum and early Holocene: evidence from Little Llangothlin Lagoon, New England Tablelands, eastern Australia
Late Pleistocene–Holocene ground surface heat flux changes reconstructed from borehole temperature data (the Urals, Russia)
Sediment sequence and site formation processes at the Arbreda Cave, NE Iberian Peninsula, and implications on human occupation and climate change during the Last Glacial
Past freeze and thaw cycling in the margin of the El'gygytgyn crater deduced from a 141 m long permafrost record
Geochronological reconsideration of the eastern European key loess section at Stayky in Ukraine
Heinrich event 4 characterized by terrestrial proxies in southwestern Europe
Tephrostratigraphic studies on a sediment core from Lake Prespa in the Balkans
Past climate changes and permafrost depth at the Lake El'gygytgyn site: implications from data and thermal modeling
Depositional dynamics in the El'gygytgyn Crater margin: implications for the 3.6 Ma old sediment archive
Coarsely crystalline cryogenic cave carbonate – a new archive to estimate the Last Glacial minimum permafrost depth in Central Europe
Hydrological variability in the Northern Levant: a 250 ka multi-proxy record from the Yammoûneh (Lebanon) sedimentary sequence
Mary Robles, Odile Peyron, Guillemette Ménot, Elisabetta Brugiapaglia, Sabine Wulf, Oona Appelt, Marion Blache, Boris Vannière, Lucas Dugerdil, Bruno Paura, Salomé Ansanay-Alex, Amy Cromartie, Laurent Charlet, Stephane Guédron, Jacques-Louis de Beaulieu, and Sébastien Joannin
Clim. Past, 19, 493–515, https://doi.org/10.5194/cp-19-493-2023, https://doi.org/10.5194/cp-19-493-2023, 2023
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Quantitative climate reconstructions based on pollen and brGDGTs reveal, for the Late Glacial, a warm Bølling–Allerød and a marked cold Younger Dryas in Italy, showing no latitudinal differences in terms of temperatures across Italy. In terms of precipitation, no latitudinal differences are recorded during the Bølling–Allerød, whereas 40–42° N appears as a key junction point between wetter conditions in southern Italy and drier conditions in northern Italy during the Younger Dryas.
Basil Andrew Stansfield Davis, Marc Fasel, Jed O. Kaplan, Emmanuele Russo, and Ariane Burke
Clim. Past Discuss., https://doi.org/10.5194/cp-2022-59, https://doi.org/10.5194/cp-2022-59, 2022
Revised manuscript accepted for CP
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During the last Ice Age 21 k BP, Northern Europe was covered in ice and steppe, and forests were restricted to sheltered regions to the south. However, the composition and extent of forest and its associated climate remains unclear, with models indicating more forest north of the Alps than suggested by the data. A new compilation of pollen records with improved dating suggests greater agreement with model climate, but still suggests models over estimate forest cover especially in the west.
Brendon J. Quirk, Elizabeth Huss, Benjamin J. C. Laabs, Eric Leonard, Joseph Licciardi, Mitchell A. Plummer, and Marc W. Caffee
Clim. Past, 18, 293–312, https://doi.org/10.5194/cp-18-293-2022, https://doi.org/10.5194/cp-18-293-2022, 2022
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Glaciers in the northern Rocky Mountains began retreating 17 000 to 18 000 years ago, after the end of the most recent global ice volume maxima. Climate in the region during this time was likely 10 to 8.5° colder than modern with less than or equal to present amounts of precipitation. Glaciers across the Rockies began retreating at different times but eventually exhibited similar patterns of retreat, suggesting a common mechanism influencing deglaciation.
Gabriella Koltai, Christoph Spötl, Alexander H. Jarosch, and Hai Cheng
Clim. Past, 17, 775–789, https://doi.org/10.5194/cp-17-775-2021, https://doi.org/10.5194/cp-17-775-2021, 2021
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This paper utilises a novel palaeoclimate archive from caves, cryogenic cave carbonates, which allow for precisely constraining permafrost thawing events in the past. Our study provides new insights into the climate of the Younger Dryas (12 800 to 11 700 years BP) in mid-Europe from the perspective of a high-elevation cave sensitive to permafrost development. We quantify seasonal temperature and precipitation changes by using a heat conduction model.
Svend Funder, Anita H. L. Sørensen, Nicolaj K. Larsen, Anders A. Bjørk, Jason P. Briner, Jesper Olsen, Anders Schomacker, Laura B. Levy, and Kurt H. Kjær
Clim. Past, 17, 587–601, https://doi.org/10.5194/cp-17-587-2021, https://doi.org/10.5194/cp-17-587-2021, 2021
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Cosmogenic 10Be exposure dates from outlying islets along 300 km of the SW Greenland coast indicate that, although affected by inherited 10Be, the ice margin here was retreating during the Younger Dryas. These results seem to be corroborated by recent studies elsewhere in Greenland. The apparent mismatch between temperatures and ice margin behaviour may be explained by the advection of warm water to the ice margin on the shelf and by increased seasonality, both caused by a weakened AMOC.
Eleanor Rainsley, Chris S. M. Turney, Nicholas R. Golledge, Janet M. Wilmshurst, Matt S. McGlone, Alan G. Hogg, Bo Li, Zoë A. Thomas, Richard Roberts, Richard T. Jones, Jonathan G. Palmer, Verity Flett, Gregory de Wet, David K. Hutchinson, Mathew J. Lipson, Pavla Fenwick, Ben R. Hines, Umberto Binetti, and Christopher J. Fogwill
Clim. Past, 15, 423–448, https://doi.org/10.5194/cp-15-423-2019, https://doi.org/10.5194/cp-15-423-2019, 2019
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The New Zealand subantarctic islands, in the Pacific sector of the Southern Ocean, provide valuable records of past environmental change. We find that the Auckland Islands hosted a small ice cap around 384 000 years ago, but that there was little glaciation during the Last Glacial Maximum, around 21 000 years ago, in contrast to mainland New Zealand. This shows that the climate here is susceptible to changes in regional factors such as sea-ice expanse and the position of ocean fronts.
Kseniia Ashastina, Lutz Schirrmeister, Margret Fuchs, and Frank Kienast
Clim. Past, 13, 795–818, https://doi.org/10.5194/cp-13-795-2017, https://doi.org/10.5194/cp-13-795-2017, 2017
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We present the first detailed description and sedimentological analyses of an 80 m permafrost sequence exposed in a mega-thaw slump near Batagay in the Yana Highlands, Russia, and attempt to deduce its genesis. First dating results (14C, OSL) show that the sequence represents a continental climate record spanning from the Middle Pleistocene to the Holocene. We suggest that the characteristics of the studied deposits are a result of various seasonally controlled climatically induced processes.
Pauline C. Treble, Andy Baker, Linda K. Ayliffe, Timothy J. Cohen, John C. Hellstrom, Michael K. Gagan, Silvia Frisia, Russell N. Drysdale, Alan D. Griffiths, and Andrea Borsato
Clim. Past, 13, 667–687, https://doi.org/10.5194/cp-13-667-2017, https://doi.org/10.5194/cp-13-667-2017, 2017
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Little is known about the climate of southern Australia during the Last Glacial Maximum and deglaciation owing to sparse records for this region. We present the first high-resolution data, derived from speleothems that grew 23–5 ka. It appears that recharge to the Flinders Ranges was higher than today, particularly during 18.9–15.8 ka, argued to be due to the enhanced availability of tropical moisture. An abrupt shift to aridity is recorded at 15.8 ka, associated with restored westerly airflow.
Andrea Catalina Gebhardt, Lieven Naudts, Lies De Mol, Jan Klerkx, Kanatbek Abdrakhmatov, Edward R. Sobel, and Marc De Batist
Clim. Past, 13, 73–92, https://doi.org/10.5194/cp-13-73-2017, https://doi.org/10.5194/cp-13-73-2017, 2017
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Seismic profiles from the western and eastern deltas of Lake Issyk-Kul were used to identify lake-level changes of up to 400 m. Seven stratigraphic sequences were identified, each containing a series of delta lobes that were formed during former lake-level stillstands. Lake-level fluctuations point to significant changes in the strength and position of the Siberian High and the mid-latitude Westerlies. Their interplay is responsible for the amount of moisture that reaches this area.
James Shulmeister, Justine Kemp, Kathryn E. Fitzsimmons, and Allen Gontz
Clim. Past, 12, 1435–1444, https://doi.org/10.5194/cp-12-1435-2016, https://doi.org/10.5194/cp-12-1435-2016, 2016
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This paper highlights that small dunes (lunettes) formed on the eastern side of a lake in the Australian sub-tropics at the height of the last ice age (about 21,000 years ago) and in the early part of the current interglacial (9–6,000 years ago). This means that it was fairly wet at these times and also that there were strong westerly winds to form the dunes. Today strong westerly winds occur in winter, and we infer that the same was also true at those times, suggesting no change in circulation.
D. Y. Demezhko and A. A. Gornostaeva
Clim. Past, 11, 647–652, https://doi.org/10.5194/cp-11-647-2015, https://doi.org/10.5194/cp-11-647-2015, 2015
M. Kehl, E. Eckmeier, S. O. Franz, F. Lehmkuhl, J. Soler, N. Soler, K. Reicherter, and G.-C. Weniger
Clim. Past, 10, 1673–1692, https://doi.org/10.5194/cp-10-1673-2014, https://doi.org/10.5194/cp-10-1673-2014, 2014
G. Schwamborn, H. Meyer, L. Schirrmeister, and G. Fedorov
Clim. Past, 10, 1109–1123, https://doi.org/10.5194/cp-10-1109-2014, https://doi.org/10.5194/cp-10-1109-2014, 2014
A. Kadereit and G. A. Wagner
Clim. Past, 10, 783–796, https://doi.org/10.5194/cp-10-783-2014, https://doi.org/10.5194/cp-10-783-2014, 2014
J. M. López-García, H.-A. Blain, M. Bennàsar, M. Sanz, and J. Daura
Clim. Past, 9, 1053–1064, https://doi.org/10.5194/cp-9-1053-2013, https://doi.org/10.5194/cp-9-1053-2013, 2013
M. Damaschke, R. Sulpizio, G. Zanchetta, B. Wagner, A. Böhm, N. Nowaczyk, J. Rethemeyer, and A. Hilgers
Clim. Past, 9, 267–287, https://doi.org/10.5194/cp-9-267-2013, https://doi.org/10.5194/cp-9-267-2013, 2013
D. Mottaghy, G. Schwamborn, and V. Rath
Clim. Past, 9, 119–133, https://doi.org/10.5194/cp-9-119-2013, https://doi.org/10.5194/cp-9-119-2013, 2013
G. Schwamborn, G. Fedorov, N. Ostanin, L. Schirrmeister, A. Andreev, and the El'gygytgyn Scientific Party
Clim. Past, 8, 1897–1911, https://doi.org/10.5194/cp-8-1897-2012, https://doi.org/10.5194/cp-8-1897-2012, 2012
K. Žák, D. K. Richter, M. Filippi, R. Živor, M. Deininger, A. Mangini, and D. Scholz
Clim. Past, 8, 1821–1837, https://doi.org/10.5194/cp-8-1821-2012, https://doi.org/10.5194/cp-8-1821-2012, 2012
F. Gasse, L. Vidal, A.-L. Develle, and E. Van Campo
Clim. Past, 7, 1261–1284, https://doi.org/10.5194/cp-7-1261-2011, https://doi.org/10.5194/cp-7-1261-2011, 2011
Cited articles
Abe-Ouchi, A., Segawa, T., and Saito, F.: Climatic Conditions for modelling the Northern Hemisphere ice sheets throughout the ice age cycle, Clim. Past, 3, 423–438, https://doi.org/10.5194/cp-3-423-2007, 2007.
\'Alvarez-Solas, J., Montoya, M., Ritz, C., Ramstein, G., Charbit, S., Dumas, C., Nisancioglu, K., Dokken, T., and Ganopolski, A.: Heinrich event 1: an example of dynamical ice-sheet reaction to oceanic changes, Clim. Past, 7, 1297–1306, https://doi.org/10.5194/cp-7-1297-2011, 2011.
Barendregt, R. W. and Irving, E.: Changes in the extent of North American ice sheets during the late Cenozoic, Can. J. Earth Sci., 35, 504–509, 1998.
Bintanja, R., van de Wal, R. S. W., and Oerlemans, J.: Global ice volume variations through the last glacial cycle simulated by a 3-D ice-dynamical model, Quaternary Int., 95–96, 11–23, 2002.
Bintanja, R. and van de Wal, R. S. W.,: North American ice-sheet dynamics and the onset of 100,000-year glacial cycles, Nature, 454, 869–872, 2008
Bonelli, S., Charbit, S., Kageyama, M., Woillez, M.-N., Ramstein, G., Dumas, C., and Quiquet, A.: Investigating the evolution of major Northern Hemisphere ice sheets during the last glacial-interglacial cycle, Clim. Past, 5, 329–345, https://doi.org/10.5194/cp-5-329-2009, 2009.
Boulton, G. S. and Clark, C. D.: A highly mobile Laurentide ice sheet revealed by satellite images of glacial lineations, Nature, 346, 813–817, 1990.
Braithwaite, R. J. and Olesen, O. B.: Calculation of glacier ablation from air-temperature, West Greenland, in: Glacier fluctuations and climatic change, edited by: Oerlemans, J., Book Series: Glaciology and Quaternary Geology, University of Utrecht, Vol. 6, 219–233, 1989.
Charbit, S., Ritz, C., Philippon, G., Peyaud, V., and Kageyama, M.: Numerical reconstructions of the Northern Hemisphere ice sheets through the last glacial-interglacial cycle, Clim. Past, 3, 15–37, https://doi.org/10.5194/cp-3-15-2007, 2007.
Clague, J. J.: Quaternary geology of the Canadian Cordillera, in: Quaternary Geology of Canada and Greenland, edited by: Fulton, R. J., Geological Society of America, Boulder, CO, 15–95, 1989.
Clark, P. U., Clague, J. J., Curry, B. B., Dreimanis, A., Hicock, S. R., Miller, G. H., Berger, G. W., Eyles, N., Lamothe, M., Miller, B. B., Mott, R. J., Oldale, R. N., Stea, R. R., Szabo, J. P., Thorleifson, L. H., and Vincent, J.-S.: Initiation and development of the Laurentide and Cor-dilleran Ice Sheets following the last interglaciation, Quaternary Sci. Rev., 12, 79–114, 1993.
Clark, P. U., Licciardi, J. M., MacAyeal, D. R., and Jenson, J. W.: Numerical reconstruction of a soft-bedded Laurentide during the Last Glacial Maximum, Geology, 24, 679–682, 1996.
Cook, K. H. and Held, I. M.: Stationary Waves of the Ice Age Climate, J. Climate, 1, 807–819, 1988.
Denton, G. H. and Hughes, T. J. (Eds.): The Last Great Ice Sheets, Wiley-Interscience, New York, 484 pp., 1981.
Dredge, L. A. and Thorleifson, H.: The Middle Wisconsinan history of the Laurentide Ice Sheet, Géographie Physique et Quaternaire, 41, 215–235, 1987.
Dyke, A. S., Andrews, J. T., Clark, P. U., England, J. H., Miller, G. H., Shaw, J., and Veillette, J. J.: The Laurentide and Innuitian ice sheets during the last glacial maximum, Quaternary Sci. Rev., 21, 9–31, 2002.
Ehlers, J. and Gibbard, P. L.: The extent and chronology of glaciations, Quaternary Sci. Rev., 22, 15–17, 2003.
England, J., Atkinson, N., Bednarski, J., Dyke, A. S., Hodgson, D. A., and Ó Cofaigh, C.: The Innuitian Ice Sheet: configuration, dynamics and chronology, Quaternary Sci. Rev., 25, 689–703, 2006.
EPICA Community Members: One-to-one coupling of glacial climate variability in Greenland and Antarctica, Nature, 444, 195–198, 2006.
Fastook, J. L. and Chapman, J.: A map plane finite-element model: Three modeling experiments, J. Glaciol., 35, 48–52, 1989.
Fastook, J. L.: The finite-element method for solving conservation equations in glaciology, Comput. Sci. Eng., 1, 55–67, 1993.
Fastook, J. L. and Prentice, M.: A finite-element model for Antarctica; Sensitivity test for meteorological mass-balance relationship, J. Glaciol., 40, 167–175, 1994.
Gregoire, L. J., Payne, A. J., and Valdes, P. J.: Deglacial rapid sea-level rises caused by ice-sheet saddle collapses, Nature, 487, 219–222, 2012.
Held, I. M., Ting, M., and Wang, H.: Northern Winter Stationary Waves: Theory and Modeling, J. Climate, 15–16, 2125–2144, 2002.
Helmens, K. and Engels, S.: Ice-free conditions in eastern Fennoscandia during early Marine Isotope Stage 3: lacustrine records, Quaternary Sci. Rev., 39, 399–409, 2010.
Holmlund, P. and Fastook, J. L.: A time dependent glaciological model of the Weichselian ice sheet, Quaternary Int., 27, 53–58, 1995.
Huybrechts, P.: A 3-D model for the Antarctic Ice Sheet: A sensitivity study on the glacial-interglacial contrast, Clim. Dynam., 5, 79–92, 1990.
Huybrechts, P. and T'siobbel, S.: Thermomechanical modelling of Northern Hemisphere ice sheets with a two-level mass-balance parameterization, Ann. Glaciol., 21, 111–116, 1995.
Imbrie, J., Harys, J. D., Martinson, D. G., McIntyre, A., Mix, A. C., Morley, J. J., Pisias, N. G., Prell, W. I., and Shackleton, N. J.: The orbital theory of Pleistocene climate: Support from revised chronology of the marine δ18O record, in: Milankovitch and Climate, edited by: Berger, A. I., Imbrie, J., Hays, J., Kukla, G., and Saltzman, B., Part 1. Reidel, Dordrecht, 269–305, 1984.
Imbrie, J. Z., Imbrie-Moore, A., and Lisiecki, L. E.: A phase-space model for Pleistocene ice volume, Earth Planet. Sci. Lett., 307, 94–102, 2011.
Johnsen, S. J., Clausen, H. B., Dansgaard, W., Gundestrup, N. S., Hammer, C. U., Andersen, U., Andersen, K. K., Hvidberg, C. S., Dahl-Jensen, D., Steffensen, J. P., Shoji, H., Sveinbjörnsdóttir, A. E., White, J. W. C., Jouzel, J., and Fisher, D.: The δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability, J. Geophys. Res., 102, 26397–26410, 1997.
Johnson, J. and Fastook, J. L.: Northern Hemisphere glaciation and its sensitivity to basal melt water, Quaternary Int., 95–96, 65–74, 2002.
Kageyama, M., Valdes, P. J., Ramstein, G., Hewitt, C., and Wyputta, U.: Northern Hemisphere Storm Tracks in Present Day and Last Glacial Maximum Climate Simulations: A comparison of the European PMIP Models, J. Climate, 12, 742–760, 1999.
Kleman, J., Hättestrand, C., Borgström, I., and Stroeven, A. P.: Fennoscandian paleoglaciology reconstructed using a glacial geological inversion model, J. Glaciol., 43, 283–299, 1997.
Kleman, J., Jansson, K. N., De Angelis, H., Stroeven, A. P., Hättestrand, C., Alm, G., and Glasser, N. F.: North American Ice Sheet build-up during the last glacial cycle 115–21 kyr, Quaternary Sci. Rev., 29, 2036–2051, 2010.
Kleman, J., Fastook, J., and Stroeven, A.: Geologically and geomopholocally constrainednumerical model of Laurentide Ice Sheet inception and build-up, Quaternary Int., 95–96, 87–98, 2002.
Kleman, J. and Hättestrand, C.: Frozen-based Fennoscandian and Laurentide ice sheets during the last glacial maximum, Nature, 402, 63–66, 1999.
Lambeck, K., Esat, T. M., and Potter, E. M.: Links between climate ansd sea-levels for the past three million years, Nature, 419, 199–206, 2002.
Lambeck, K., Purcell, A., Funder, S., Kjær, K. H., Larsen, E., and Möller, P.: Constraints on the Late Saalian to early Middle Weichselian ice sheet of Eurasia from field data and rebound modelling, Boreas, 35, 539–575, 2006.
Landwehr, J. M., Coplen, T. B., Ludwig, K. R., Winograd, I. J., and Riggs, A.: Data from Devils Hole Core DH-11, USGS Open File Rep. 97–792, USGS, Washington D.C., 1997.
Langen, P. L. and Vinther, B. M.: Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions, Clim. Dynam., 32, 1035–1054, 2009.
Liakka, J. and Nilsson, J.: The impact of topographically forced stationary waves on local ice sheet climate, J. Glaciol., 56, 534–544, 2010.
Liakka, J., Nilsson, J., and Löfverström, M.: Interactions between stationary waves and ice sheets: linear versus nonlinear atmospheric response, Clim. Dynam., 37, 531–553, https://doi.org/10.1007/s00382-011-1004-6, 2011.
Lisiecki, L. E. and Raymo, M. E.: A Pliocene-Pleistocene stack of 57 globally distributed bethic δ18O records, Paleoceanography, 20, https://doi.org/10.1029/2004PA001071, 2005.
Ljungner, E.: East-west balance of the Quaternary ice caps in Patagonia and Scandinavia. Buletin of the Geological Institute, Uppsala, 33, 1–96, 1949.
Lourens, L. J., Becker, J., Bintanja, R., Hilgen, F. J., Tuenter, E., van de Wal, R. S. W., and Ziegler, M.: Linear and non-linear response of the late Neogene glacial cycles to obliquity forcing and implications for the Milankovitch theory, Quaternary Sci. Rev., 29, 352–365, 2010.
Lundqvist, J.: Glacial history of Sweden, in: Quaternary glaciations – Extent and Chronology, edited by: Ehlers, J. and Gibbard, P. L., Vol. 1. Europe, Elsevier, Amsterdam, 2004.
Ma, Y., Gagliardini, O., Ritz, C., Gillet-Chaulet, F., Durand, G., and Montagnat, M.: Enhancement factors for grounded ice and ice shelves inferred from an anisotropic ice-flow model, J. Glaciol., 56, 805–812, 2010.
Manabe, S. and Broccoli, A. J.: The influence of continental ice sheets on the climate of an ice age, J. Geophys. Res., 90, 2167–2190, 1985.
Mangerud, J.: Ice sheet limits in Norway and on the Norwegian continental shelf, in: Quaternary glaciations – Extent and Chronology, edited by: Ehlers, J. and Gibbard, P. L., Vol.. 1, Europe, Elsevier, Amsterdam, 2004.
Marshall, S. J., Tarasov, L., Clarke, G. K. C., and Peltier, W. R.: Glaciological reconstruction of the Laurentide Ice Sheet: Physical processes and modelling challenges, Can. J. Earth Sci., 37, 769–793, 2000.
McMartin, I. and Henderson, P. J.: Evidence from Keewatin (central Nunavut) for paleo-ice divide migration, Géographie Physique et Quaternaire, 58, 163–186, 2004.
Otieno, F. O. and Bromwich, D. H.: Contribution of Atmospheric Circulation to Inception of the Laurentide Ice Sheet at 116 kyr BP, J. Climate, 22, 39–57, 2009.
Otto-Bliesner, B. L., Brady, E. C., Clauzet, G., Tomas, R., Levis, S., and Kothavala, Z.: Last Glacial Maximum and Holocene Climate in CCSM3, J. Climate, 19, 2526–2544, 2006.
Paterson, W. S. B.: The physics of glaciers, 3rd Edn., Pergamon, Oxford, 1994.
Peltier, W. R.: Global Glacial Isostasy and the Surface of Ice-Age earth: The ICE-5G (VM2) Model and GRACE, Ann. Rev. Earth Planet. Sci., 32, 111–149, 2004.
Petit, J. R., Jouzel, J., Raynaud, D., Barkov, N. I., Barnola, J.-M., Basile, I., Benders, M., Chappellaz, J., Davis, M., Delayque, G., Delmotte, M., Kotlyakov, V. M., Legrand, M., Lipenkov, V. Y., Lorius, C., Pépin, L., Ritz, C., Saltzman, E., and Stievenard, M.: Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica, Nature 399, 429–436, 1999.
Roe, G. H. and Lindzén, R. S.: The mutual Interaction between Continental-Scale Ice Sheets and Atmospheric Stationary Waves, J. Climate, 14, 1450–1465, 2001.
Stea, R. R.: The Appalachian glacier Complex in Maritime Canada, in Quaternary Glaciations – Extent and Chronology, Part II: North America, edited by: Ehlers, J. and Gibbard, P. L., Elsevier, Amsterdam, 213–232, 2004.
Stokes, C. R., Tarasov, L., and Dyke, A. S.: Dynamics of the North American Ice Sheet Complex during its inception and build-up to the last glacial maximum, Quaternary Sci. Rev., 50, 86–104, 2012.
Stumpf, A. J., Broster, B. E., and Levson, V. M.: Multiphase flow of the Late Wisconsinan Cordilleran ice sheet in western Canada, Geol. Soc. Am. Bull., 112, 1850–1863, 2000.
Svendsen, J. I., Alexanderson, H., Astakhov, V. I., Demidov, I., Dowdeswell, J. A., Funder, S., Gataullin, V., Henriksen, M., Hjort, C., Houmark-Nielsen, M., Hubberten, H. W., Ingolfsson, O., Jakobsson, M., Kjaer, K. H., Larsen, E., Lokrantz, H., Lunkka, J. P. Lyså, A., Mangerud, J., Matiouchkov, A., Murray, A., Moller, P., Niessen, F., Nikolskaya, O., Polyak, L., Saarnisto, M., Siegert, C., Siegert, M. J., Spielhagen, R. F., and Stein, R.: Late Quaternary ice sheet history of northern Eurasia, Quaternary Sci. Rev., 23, 1229–1271, 2004.
Svensson, A., Bigler, M., Blunier, T., Clausen, H. B., Dahl-Jensen, D., Fischer, H., Fujita, S., Goto-Azuma, K., Johnsen, S. J., Kawamura, K., Kipfstuhl, S., Kohno, M., Parrenin, F., Popp, T., Rasmussen, S. O., Schwander, J., Seierstad, I., Severi, M., Steffensen, J. P., Udisti, R., Uemura, R., Vallelonga, P., Vinther, B. M., Wegner, A., Wilhelms, F., and Winstrup, M.: Direct linking of Greenland and Antarctic ice cores at the Toba eruption (74 ka BP), Clim. Past, 9, 749–766, https://doi.org/10.5194/cp-9-749-2013, 2013.
Tarasov, L. and Peltier, W. R.: A geophysically constrained large ensemble analysis of the deglacial history of the North American ice-sheet complex, Quaternary Sci. Rev., 23, 359–388, 2004.
Ukkonen, P., Arppe, L., Houmark-Nielsen, M., Kjaer, K. H., and Karhu, J. A.: MIS 3 Mammoth remains from Sweden – implications for faunal history and paleoclimate and glaciation chronology, Quaternary Sci. Rev., 26, 3081–3098, 2003.
Weertman, J.: Deformation of floating ice shelves, J. Glaciol., 3, 38–42, 1957.
Weertman, J.: The theory of glacier sliding, J. Glaciol., 5, 287–303, 1964.
Weertman, J.: Water lubrication mechanism of glacier surges, Can. J. Earth Sci., 6, 929–942, 1969.
Weertman, J. and Birchfield, G. E.: Subglacial water flow under ice streams and West Anterctic ice sheet stability, Ann. Glaciol., 3, 316–320, 1982.
Winsborrow, M., Clark, C., and Stokes, C.: Ice streams of the Laurentide ice sheet, Ge\`iographie Physique et Quaternaire, 58, 269–280, 2004.
Wohlfarth, B.: Ice-free conditions in Sweden during Marine Oxygen Isotope Stage 3?, Boreas, 39, 377–398, 2010.