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  • 1
    Publication Date: 2015-12-18
    Description: The response of the Greenland Ice Sheet (GIS) to changes in temperature during the twentieth century remains contentious, largely owing to difficulties in estimating the spatial and temporal distribution of ice mass changes before 1992, when Greenland-wide observations first became available. The only previous estimates of change during the twentieth century are based on empirical modelling and energy balance modelling. Consequently, no observation-based estimates of the contribution from the GIS to the global-mean sea level budget before 1990 are included in the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Here we calculate spatial ice mass loss around the entire GIS from 1900 to the present using aerial imagery from the 1980s. This allows accurate high-resolution mapping of geomorphic features related to the maximum extent of the GIS during the Little Ice Age at the end of the nineteenth century. We estimate the total ice mass loss and its spatial distribution for three periods: 1900-1983 (75.1 +/- 29.4 gigatonnes per year), 1983-2003 (73.8 +/- 40.5 gigatonnes per year), and 2003-2010 (186.4 +/- 18.9 gigatonnes per year). Furthermore, using two surface mass balance models we partition the mass balance into a term for surface mass balance (that is, total precipitation minus total sublimation minus runoff) and a dynamic term. We find that many areas currently undergoing change are identical to those that experienced considerable thinning throughout the twentieth century. We also reveal that the surface mass balance term shows a considerable decrease since 2003, whereas the dynamic term is constant over the past 110 years. Overall, our observation-based findings show that during the twentieth century the GIS contributed at least 25.0 +/- 9.4 millimetres of global-mean sea level rise. Our result will help to close the twentieth-century sea level budget, which remains crucial for evaluating the reliability of models used to predict global sea level rise.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kjeldsen, Kristian K -- Korsgaard, Niels J -- Bjork, Anders A -- Khan, Shfaqat A -- Box, Jason E -- Funder, Svend -- Larsen, Nicolaj K -- Bamber, Jonathan L -- Colgan, William -- van den Broeke, Michiel -- Siggaard-Andersen, Marie-Louise -- Nuth, Christopher -- Schomacker, Anders -- Andresen, Camilla S -- Willerslev, Eske -- Kjaer, Kurt H -- England -- Nature. 2015 Dec 17;528(7582):396-400. doi: 10.1038/nature16183.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Centre for GeoGenetics, Natural History Museum, University of Copenhagen, Copenhagen 1350, Denmark. ; Department of Earth Sciences, University of Ottawa, Ottawa, Ontario K1N 6N5, Canada. ; DTU Space-National Space Institute, Technical University of Denmark, Department of Geodesy, Kongens Lyngby 2800, Denmark. ; Geological Survey of Denmark and Greenland, Department of Marine Geology and Glaciology, Copenhagen 1350, Denmark. ; Department of Geoscience, Aarhus University, Aarhus 8000, Denmark. ; Bristol Glaciology Centre, University of Bristol, Bristol BS8 1SS, UK. ; Department of Earth and Space Science and Engineering, York University, Toronto, Ontario M3J 1P3, Canada. ; Institute for Marine and Atmospheric Research, Utrecht University, Utrecht 80005, The Netherlands. ; Department of Geosciences, University of Oslo, Oslo 0316, Norway.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26672555" target="_blank"〉PubMed〈/a〉
    Keywords: Climate Change/*statistics & numerical data ; Greenland ; History, 20th Century ; History, 21st Century ; *Ice Cover ; Models, Theoretical ; Observation ; Photography ; Reproducibility of Results ; Seawater/analysis ; *Spatio-Temporal Analysis ; Temperature
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2011-08-06
    Description: We present a sea-ice record from northern Greenland covering the past 10,000 years. Multiyear sea ice reached a minimum between ~8500 and 6000 years ago, when the limit of year-round sea ice at the coast of Greenland was located ~1000 kilometers to the north of its present position. The subsequent increase in multiyear sea ice culminated during the past 2500 years and is linked to an increase in ice export from the western Arctic and higher variability of ice-drift routes. When the ice was at its minimum in northern Greenland, it greatly increased at Ellesmere Island to the west. The lack of uniformity in past sea-ice changes, which is probably related to large-scale atmospheric anomalies such as the Arctic Oscillation, is not well reproduced in models. This needs to be further explored, as it is likely to have an impact on predictions of future sea-ice distribution.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Funder, Svend -- Goosse, Hugues -- Jepsen, Hans -- Kaas, Eigil -- Kjaer, Kurt H -- Korsgaard, Niels J -- Larsen, Nicolaj K -- Linderson, Hans -- Lysa, Astrid -- Moller, Per -- Olsen, Jesper -- Willerslev, Eske -- New York, N.Y. -- Science. 2011 Aug 5;333(6043):747-50. doi: 10.1126/science.1202760.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Centre for GeoGenetics, Natural History Museum of Denmark, University of Copenhagen, Oster Voldgade 5-7, DK 1350 Copenhagen K, Denmark. svf@snm.ku.dk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21817051" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2012-08-04
    Description: Global warming is predicted to have a profound impact on the Greenland Ice Sheet and its contribution to global sea-level rise. Recent mass loss in the northwest of Greenland has been substantial. Using aerial photographs, we produced digital elevation models and extended the time record of recent observed marginal dynamic thinning back to the mid-1980s. We reveal two independent dynamic ice loss events on the northwestern Greenland Ice Sheet margin: from 1985 to 1993 and 2005 to 2010, which were separated by limited mass changes. Our results suggest that the ice mass changes in this sector were primarily caused by short-lived dynamic ice loss events rather than changes in the surface mass balance. This finding challenges predictions about the future response of the Greenland Ice Sheet to increasing global temperatures.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kjaer, Kurt H -- Khan, Shfaqat A -- Korsgaard, Niels J -- Wahr, John -- Bamber, Jonathan L -- Hurkmans, Ruud -- van den Broeke, Michiel -- Timm, Lars H -- Kjeldsen, Kristian K -- Bjork, Anders A -- Larsen, Nicolaj K -- Jorgensen, Lars Tyge -- Faerch-Jensen, Anders -- Willerslev, Eske -- New York, N.Y. -- Science. 2012 Aug 3;337(6094):569-73. doi: 10.1126/science.1220614.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Centre for GeoGenetics, Natural History Museum, University of Copenhagen, Copenhagen, Denmark. kurtk@snm.ku.dk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22859486" target="_blank"〉PubMed〈/a〉
    Keywords: Computer Simulation ; *Global Warming ; Greenland ; *Ice Cover ; Models, Theoretical ; Photography
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2017-12-19
    Description: Changes in Greenland’s peripheral glaciers linked to the North Atlantic Oscillation Changes in Greenland’s peripheral glaciers linked to the North Atlantic Oscillation, Published online: 18 December 2017; doi:10.1038/s41558-017-0029-1 Combining historical aerial surveys, expedition photographs, and both spy and modern satellite imagery reveals a pronounced retreat of peripheral glaciers in east and west Greenland, linked to changes in precipitation associated with the NAO.
    Print ISSN: 1758-678X
    Electronic ISSN: 1758-6798
    Topics: Geosciences
    Published by Springer Nature
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  • 5
    Publication Date: 2014-08-18
    Description: Observations over the past decade show significant ice loss associated with the speed-up of glaciers in southeast Greenland from 2003, followed by a deceleration from 2006. These short-term, episodic, dynamic perturbations have a major impact on the mass balance on the decadal scale. To improve the projection of future sea level rise, a long-term data record that reveals the mass balance beyond such episodic events is required. Here, we extend the observational record of marginal thinning of Helheim and Kangerdlugssuaq glaciers from 10 to more than 80 years. We show that, although the frontal portion of Helheim Glacier thinned by more than 100 m between 2003 and 2006, it thickened by more than 50 m during the previous two decades. In contrast, Kangerdlugssuaq Glacier underwent minor thinning of 40–50 m from 1981 to 1998 and major thinning of more than 100 m after 2003. Extending the record back to the end of the Little Ice Age (prior to 1930) shows no thinning of Helheim Glacier from its maximum extent during the Little Ice Age to 1981, while Kangerdlugssuaq Glacier underwent substantial thinning of 230 to 265 m. Comparison of sub-surface water temperature anomalies and variations in air temperature to records of thickness and velocity change suggest that both glaciers are highly sensitive to short-term atmospheric and ocean forcing, and respond very quickly to small fluctuations. On century timescales, however, multiple external parameters (e.g. outlet glacier shape) may dominate the mass change. These findings suggest that special care must be taken in the projection of future dynamic ice loss.
    Print ISSN: 1994-0416
    Electronic ISSN: 1994-0424
    Topics: Geography , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 6
    Publication Date: 2014-02-21
    Description: Observations over the past decade show significant ice loss associated with the speed-up of glaciers in southeast Greenland from 2003, followed by a deceleration from 2006. These short-term, episodic, dynamic perturbations have a major impact on the mass balance at the decadal scale. To improve the projection of future sea level rise, a long-term data record that reveals the mass balance beyond such episodic events is required. Here, we extend the observational record of marginal thinning of Helheim glacier (HG) and Kangerdlugssuaq glacier (KG) from 10 to more than 150 yr. We show that although the frontal portion of HG thinned by more than 100 m between 2003 and 2006, it thickened by more than 50 m during the previous two decades. In contrast, KG was stable from 1981 to 1998 and experienced major thinning only after 2003. Extending the record back to the end of the Little Ice Age (ca. 1850) shows no significant thinning of HG from 1850 to 1981, while KG underwent substantial thinning of ~265 m. Analyses of their sensitivity to sub-surface water temperature anomalies and variations in air temperature suggest that both HG and KG are highly sensitive to short-term atmospheric and ocean forcing, and respond very quickly to small fluctuations. At century time-scales, however, multiple external parameters (e.g. outlet shape) dominate the mass change. These findings undermine attempts to use measurements over the last decade as initial conditions to project future dynamic ice loss.
    Print ISSN: 1994-0432
    Electronic ISSN: 1994-0440
    Topics: Geography , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 7
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