Relevant bibliographies by topics / Greenland ice sheet melting

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Greenland ice sheet melting'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Greenland ice sheet melting"

1

Slater, Donald A., Fiamma Straneo, Denis Felikson, et al. "Estimating Greenland tidewater glacier retreat driven by submarine melting." Cryosphere 13, no. 9 (2019): 2489–509. http://dx.doi.org/10.5194/tc-13-2489-2019.

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Abstract. The effect of the North Atlantic Ocean on the Greenland Ice Sheet through submarine melting of Greenland's tidewater glacier calving fronts is thought to be a key driver of widespread glacier retreat, dynamic mass loss and sea level contribution from the ice sheet. Despite its critical importance, problems of process complexity and scale hinder efforts to represent the influence of submarine melting in ice-sheet-scale models. Here we propose parameterizing tidewater glacier terminus position as a simple linear function of submarine melting, with submarine melting in turn estimated as
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Slater, Thomas, Isobel R. Lawrence, Inès N. Otosaka, et al. "Review article: Earth's ice imbalance." Cryosphere 15, no. 1 (2021): 233–46. http://dx.doi.org/10.5194/tc-15-233-2021.

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Abstract. We combine satellite observations and numerical models to show that Earth lost 28 trillion tonnes of ice between 1994 and 2017. Arctic sea ice (7.6 trillion tonnes), Antarctic ice shelves (6.5 trillion tonnes), mountain glaciers (6.1 trillion tonnes), the Greenland ice sheet (3.8 trillion tonnes), the Antarctic ice sheet (2.5 trillion tonnes), and Southern Ocean sea ice (0.9 trillion tonnes) have all decreased in mass. Just over half (58 %) of the ice loss was from the Northern Hemisphere, and the remainder (42 %) was from the Southern Hemisphere. The rate of ice loss has risen by 57
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Liu, Jiping, Zhiqiang Chen, Jennifer Francis, Mirong Song, Thomas Mote, and Yongyun Hu. "Has Arctic Sea Ice Loss Contributed to Increased Surface Melting of the Greenland Ice Sheet?" Journal of Climate 29, no. 9 (2016): 3373–86. http://dx.doi.org/10.1175/jcli-d-15-0391.1.

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Abstract In recent decades, the Greenland ice sheet has experienced increased surface melt. However, the underlying cause of this increased surface melting and how it relates to cryospheric changes across the Arctic remain unclear. Here it is shown that an important contributing factor is the decreasing Arctic sea ice. Reduced summer sea ice favors stronger and more frequent occurrences of blocking-high pressure events over Greenland. Blocking highs enhance the transport of warm, moist air over Greenland, which increases downwelling infrared radiation, contributes to increased extreme heat eve
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Li, Siqi. "Modeling the Impact of Greenland Ice Sheet Melting on Global Sea Level Elevation and Climate Change Feedback Mechanisms." Theoretical and Natural Science 86, no. 1 (2025): 126–33. https://doi.org/10.54254/2753-8818/2025.20193.

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The rapid acceleration of global warming is leading to an increased rate of glacier melt at the Earth's poles, which exacerbates the threats posed by the climate crisis and contributes to rising ocean levels. The Greenland Ice Sheet, recognized as the second-largest ice sheet globally, has housed its extensive glaciers and ice caps for at least 18 million years [1]. The melting and potential collapse of this ice sheet could significantly affect Worldwide climate and sea height. This research aims to develop a coupled model to assess rising sea levels caused by the thawing of the Greenland Ice
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Smith, Ben, Helen A. Fricker, Alex S. Gardner, et al. "Pervasive ice sheet mass loss reflects competing ocean and atmosphere processes." Science 368, no. 6496 (2020): 1239–42. http://dx.doi.org/10.1126/science.aaz5845.

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Quantifying changes in Earth’s ice sheets and identifying the climate drivers are central to improving sea level projections. We provide unified estimates of grounded and floating ice mass change from 2003 to 2019 using NASA’s Ice, Cloud and land Elevation Satellite (ICESat) and ICESat-2 satellite laser altimetry. Our data reveal patterns likely linked to competing climate processes: Ice loss from coastal Greenland (increased surface melt), Antarctic ice shelves (increased ocean melting), and Greenland and Antarctic outlet glaciers (dynamic response to ocean melting) was partially compensated
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Braithwaite, R. J., N. Reeh, and A. Weidick. "Greenland glaciers and the 'greenhouse effect', status 1991." Rapport Grønlands Geologiske Undersøgelse 155 (January 1, 1992): 9–13. http://dx.doi.org/10.34194/rapggu.v155.8171.

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Possible global climate change caused by increased 'greenhouse effect' continues to be a matter of international public concern. In particular, a warmer climate is expected to cause increased melting of the Greenland ice sheet, and a rise in world sea level. The Greenland ice sheet is therefore a potential hazard for low-Iying countries. Climate warming may be apparent first, and with greatest magnitude, at high latitudes so that increased melting of the Greenland ice sheet could give early warning of global climate change. For these reasons, GGU and foreign organisations are studying Greenlan
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Wang, Hejing, Dehai Luo, Yanan Chen, and Yao Ge. "Spatially Heterogeneous Effects of Atmospheric Circulation on Greenland Ice Sheet Melting." Atmosphere 15, no. 1 (2023): 57. http://dx.doi.org/10.3390/atmos15010057.

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The melting of the Greenland ice sheet (GrIS) in summer has rapidly and significantly increased in recent decades, especially for the northern GrIS. Circulation related to GrIS melting is important for understanding the contribution of the GrIS to the global sea level. In this paper, we used the SOM method to obtain three spatial patterns of GrIS melting based on model output data: overall melting, northern melting, and southern melting patterns. We also examined their linkages to the observed atmospheric circulation. GrIS melting is primarily related to Greenland blocking (GB), while differen
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Braithwaite, R. J., O. B. Olesen, N. Reeh, and A. Weidick. "Greenland glaciers and the 'greenhouse effect', activities 1993." Rapport Grønlands Geologiske Undersøgelse 160 (January 1, 1994): 80–82. http://dx.doi.org/10.34194/rapggu.v160.8236.

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Possible global climate change caused by increased 'greenhouse effect' may lead to a warmer climate that will cause increased melting of the Greenland ice sheet, and a rise in world sea level. Climate warming may be apparent first and with greatest magnitude at high latitudes so that increased melting of the Greenland ice sheet could give early warning of global climate change. For these reasons, GGU and foreign organisations are studying Greenland glaciers in connection with the ‘greenhouse effect’ (Braithwaite et al. 1992).
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Quiquet, A., C. Ritz, H. J. Punge, and D. Salas y Mélia. "Greenland ice sheet contribution to sea level rise during the last interglacial period: a modelling study driven and constrained by ice core data." Climate of the Past 9, no. 1 (2013): 353–66. http://dx.doi.org/10.5194/cp-9-353-2013.

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Abstract. As pointed out by the forth assessment report of the Intergovernmental Panel on Climate Change, IPCC-AR4 (Meehl et al., 2007), the contribution of the two major ice sheets, Antarctica and Greenland, to global sea level rise, is a subject of key importance for the scientific community. By the end of the next century, a 3–5 °C warming is expected in Greenland. Similar temperatures in this region were reached during the last interglacial (LIG) period, 130–115 ka BP, due to a change in orbital configuration rather than to an anthropogenic forcing. Ice core evidence suggests that the Gree
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Slater, Donald A., Denis Felikson, Fiamma Straneo, et al. "Twenty-first century ocean forcing of the Greenland ice sheet for modelling of sea level contribution." Cryosphere 14, no. 3 (2020): 985–1008. http://dx.doi.org/10.5194/tc-14-985-2020.

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Abstract. Changes in ocean temperature and salinity are expected to be an important determinant of the Greenland ice sheet's future sea level contribution. Yet, simulating the impact of these changes in continental-scale ice sheet models remains challenging due to the small scale of key physics, such as fjord circulation and plume dynamics, and poor understanding of critical processes, such as calving and submarine melting. Here we present the ocean forcing strategy for Greenland ice sheet models taking part in the Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6), the primary communi
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Dissertations / Theses on the topic "Greenland ice sheet melting"

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Slater, Donald Alexander. "Modelling submarine melting at tidewater glaciers in Greenland." Thesis, University of Edinburgh, 2017. http://hdl.handle.net/1842/28899.

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The recent thinning, acceleration and retreat of tidewater glaciers around Greenland suggests that these systems are highly sensitive to a change in climate. Tidewater glacier dynamics have already had a significant impact on global sea level, and, given projected future climate warming, will likely continue to do so over the coming century. Understanding of the processes connecting climatic change to tidewater glacier response is, however, at an early stage. Current leading thinking links tidewater glacier change to ocean warming by submarine melting of glacier calving fronts, yet the process
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Johansson, A. Malin. "Remote sensing of supra-glacial lakes on the west Greenland Ice Sheet." Doctoral thesis, Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK), 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-74509.

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The Greenland Ice Sheet is the largest ice sheet in the northern hemisphere. Ongoing melting of the ice sheet, resulting in increased mass loss relative to the longer term trend, has raised concerns about the stability of the ice sheet. Melt water generated at the surface is temporarily stored in supra-glacial lakes on the ice sheet. Connections between melt water generation, storage and ice sheet dynamics highlight the importance of the surface hydrological system. In this thesis different methods are used that improve our ability to observe the supra-glacial lake system on the west Greenland
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Beadling, Rebecca Lynn. "Impact of the Melting of the Greenland Ice Sheet on the Atlantic Meridional Overturning Circulation in 21st Century Model Projections." Thesis, The University of Arizona, 2016. http://hdl.handle.net/10150/613379.

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Contemporary observations show an increase in the melting of the Greenland Ice Sheet (GrIS) since the early 21st century. Located near the critical sites of oceanic deep convection and deep water formation, the melting of the GrIS has the potential to directly impact the Atlantic Meridional Overturning Circulation (AMOC) by freshening ocean surface waters in these regions. The majority of the Coupled Model Intercomparison Project Phase 5 (CMIP5) models project a decline in AMOC strength by 10-50% during the 21st century, in response to the increase in atmospheric greenhouse gas (GHG) concentra
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Bhattacharya, Indrajit. "ANALYSIS OF SURFACE MELTING AND SNOW ACCUMULATION OVER THE GREENLAND ICE SHEET FROM SPACEBORNE MICROWAVE SENSORS." The Ohio State University, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=osu1276621670.

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Hulton, Nicholas R. J. "Modelling the Greenland ice sheet." Thesis, University of Edinburgh, 1992. http://hdl.handle.net/1842/19859.

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A dynamic, vertically integrated, three-dimensional, mass continuity, computer model of the Greenland ice sheet is used to predict the ice sheet's response to climatic perturbation. The ice flow is gravity driven according to glaciological physics, whereby ice flow is claculated as the sum of deformation and sliding components averaged over the ice thickness where longitudinal stresses are considered negligible. The model has inputs of the present-day ice surface and basal topography, and is forced by changes in sea level and surface mass balance, which are modelled by separately described and
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Butler, Catriona Elizabeth Hamilton. "Hydrochemistry of the Greenland Ice Sheet." Thesis, University of Bristol, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.683692.

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The subglacial environment of the Greenland Ice Sheet (GrIS) is poorly understood, in terms of hydrology, water storage and biogeochemical processes. High temporal resolution biogeochemical sampling of bulk meltwaters at a typical, land-terminating outlet glacier of the GrIS was employed in order to infer processes at the ice sheet bed over three contrasting melt seasons. No high temporal resolution geochemical datasets previously existed for ice sheet environments, mainly due to inaccessibility. Bulk meltwaters comprised differing propOltions of waters originating from a widespread, distribut
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Tedstone, Andrew Jachnik. "Hydrological controls on Greenland Ice Sheet motion." Thesis, University of Edinburgh, 2015. http://hdl.handle.net/1842/14169.

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An improved understanding of the processes controlling the dynamics of the Greenland Ice Sheet is needed to enable more accurate determination of the response of the ice sheet to projected climate change. Meltwater produced on the ice sheet surface can penetrate to the bed and cause ice motion to speed up through enhanced basal sliding. However, the importance of coupled hydro-dynamics both to current ice sheet motion and future stability over the coming century is unclear. This thesis presents observations from the south-west Greenland Ice Sheet which improve our understanding of coupled hydr
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Banwell, Alison Frances. "Modelling the hydrology of the Greenland Ice Sheet." Thesis, University of Cambridge, 2013. https://www.repository.cam.ac.uk/handle/1810/267715.

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There is increasing recognition that the hydrology of the Greenland Ice Sheet plays an important role in the dynamics and therefore mass balance of the ice sheet. Understanding the hydrology of the ice sheet and being able to predict its future behaviour is therefore a key aspect of glaciological research. To date, the ice sheet’s hydrology has tended to be inferred from the analysis of surface velocity measurements, or modelled in a theoretical, idealised way. This study focuses on the development of a high spatial (100 m) and temporal (1 hour) resolution, physically based, time-dependent hyd
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Karatay, Mehmet Rahmi. "Modelling the hydrology of the Greenland ice sheet." Thesis, University of Edinburgh, 2011. http://hdl.handle.net/1842/5282.

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This thesis aims to better understand the relationships between basal water pressure, friction, and sliding mechanisms at ice sheet scales. In particular, it develops a new subglacial hydrology model (Hydro) to explicitly predict water pressures in response to basal water production and water injection from the surface. Recent research suggests that the Greenland ice sheet (gis) is losing a substantial volume of ice through dynamic thinning. This process must be modelled to accurately assess the contribution of the gis to sea-level rise in future warming scenarios. A key control on dynamic thi
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Lecavalier, Benoit. "A Model of the Greenland Ice Sheet Deglaciation." Thèse, Université d'Ottawa / University of Ottawa, 2013. http://hdl.handle.net/10393/30362.

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The goal of this thesis is to improve our understanding of the Greenland ice sheet (GrIS) and how it responds to climate change. This was achieved using ice core records to infer elevation changes of the GrIS during the Holocene (11.7 ka BP to Present). The inferred elevation changes show the response of the ice sheet interior to the Holocene Thermal Maximum (HTM; 9-5 ka BP) when temperatures across Greenland were warmer than present. These ice-core derived thinning curves act as a new set of key constraints on the deglacial history of the GrIS. Furthermore, a calibration was conducted on a th
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Books on the topic "Greenland ice sheet melting"

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Konzelmann, Thomas. Radiation conditions on the Greenland Ice Sheet. Geographisches Institut ETH, 1994.

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Qu, Bo. The Impact of Melting Ice on the Ecosystems in Greenland Sea. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-54498-9.

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Boswell, Steven M. Enhanced Surface Melting of the Fennoscandian Ice Sheet during Stadials. [publisher not identified], 2018.

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Saito, Fuyuki. Development of a three dimensional ice sheet model for numerical studies of Antarctic and Greenland ice sheet. University of Tokyo, Center for Climate System Research, 2002.

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Tōkyō Daigaku. Kikō Shisutemu Kenkyū Sentā, ed. Development of a three dimensional ice sheet model for numerical studies of Antarctic and Greenland ice sheet. University of Tokyo, Center for Climate System Research, 2002.

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A, Bindschadler R., ed. Surface topography of the Greenland ice sheet from satellite radar altimetry. National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Division, 1989.

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T, Swift Calvin, and United States. National Aeronautics and Space Administration., eds. Measuring geophysical parameters of the Greenland ice sheet using airborne radar altimetry. National Aeronautics and Space Administration, 1995.

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United States. National Aeronautics and Space Administration., ed. Operation of a radar altimeter over the Greenland ice sheet: A thesis. National Aeronautics and Space Administration, 1996.

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T, Swift Calvin, and United States. National Aeronautics and Space Administration., eds. Measuring geophysical parameters of the Greenland ice sheet using airborne radar altimetry. National Aeronautics and Space Administration, 1995.

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Chu, Wing Yin. Variability of Subglacial Drainage Across the Greenland Ice Sheet: A Joint Model/Radar Study. [publisher not identified], 2017.

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Book chapters on the topic "Greenland ice sheet melting"

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Driesschaert, E., T. Fichefet, H. Goosse, et al. "Modeling the Influence of Greenland Ice Sheet Melting on the Atlantic Meridional Overturning Circulation During the Next Millennia." In Collected Reprint Series. American Geophysical Union, 2014. http://dx.doi.org/10.1002/9781118782033.ch36.

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Swingedouw, Didier, and Pascale Braconnot. "Effect of the Greenland ice-sheet melting on the response and stability of the AMOC in the Next centuries." In Ocean Circulation: Mechanisms and Impacts—Past and Future Changes of Meridional Overturning. American Geophysical Union, 2007. http://dx.doi.org/10.1029/173gm24.

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Christoffersen, Poul. "Greenland Ice Sheet." In Encyclopedia of Earth Sciences Series. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_227.

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Yde, Jacob C. "Greenland Glaciers Outside the Ice Sheet." In Encyclopedia of Earth Sciences Series. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_643.

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Mernild, Sebastian H., Glen E. Liston, and Daqing Yang. "Greenland Ice Sheet and Arctic Mountain Glaciers." In Arctic Hydrology, Permafrost and Ecosystems. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-50930-9_5.

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Langway, C. C., H. Oeschger, and W. Dansgaard. "The Greenland Ice Sheet Program in perspective." In Greenland Ice Core: Geophysics, Geochemistry, and the Environment. American Geophysical Union, 1985. http://dx.doi.org/10.1029/gm033p0001.

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Qu, Bo. "Overview Greenland Sea." In The Impact of Melting Ice on the Ecosystems in Greenland Sea. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-54498-9_1.

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Keller, K., R. Forsberg, and C. S. Nielsen. "Kinematic GPS for Ice Sheet Surveys in Greenland." In Advances in Positioning and Reference Frames. Springer Berlin Heidelberg, 1998. http://dx.doi.org/10.1007/978-3-662-03714-0_59.

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Castello, John D., Scott O. Rogers, James E. Smith, William T. Starmer, and Yinghao Zhao. "Chapter 13. Plant and Bacterial Viruses in the Greenland Ice Sheet." In Life in Ancient Ice, edited by John D. Castello and Scott O. Rogers. Princeton University Press, 2005. http://dx.doi.org/10.1515/9781400880188-017.

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Sørensen, L. Sandberg, and R. Forsberg. "Greenland Ice Sheet Mass Loss from GRACE Monthly Models." In Gravity, Geoid and Earth Observation. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-10634-7_70.

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Conference papers on the topic "Greenland ice sheet melting"

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Hossain, Emam, Md Osman Gani, Devon Dunmire, Aneesh C. Subramanian, and Hammad Younas. "Time Series Classification of Supraglacial Lakes Evolution over Greenland Ice Sheet." In 2024 International Conference on Machine Learning and Applications (ICMLA). IEEE, 2024. https://doi.org/10.1109/icmla61862.2024.00072.

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Hossan, Alamgir, Andreas Colliander, Julie Miller, Shawn Marshall, Joel Harper, and Baptiste Vandecrux. "Estimation of Total Surface and Subsurface Meltwater Amounts Across Greenland Ice Sheet." In IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10641900.

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Ji, Changdong, Jiarong Yang, and Guanmei Chen. "Piecewise polynomial fitting of the mass change trend of the Greenland ice sheet." In Third International Conference on Environmental Remote Sensing and Geographic Information Technology (ERSGIT 2024), edited by Kun Tan and Guobiao Yao. SPIE, 2025. https://doi.org/10.1117/12.3059585.

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McCutcheon, Jenine, James B. McQuaid, Christopher Williamson, et al. "Aerosols and Albedo: Links between Airborne Particulate Matter and Melting of the Greenland Ice Sheet." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1756.

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Dods, Melissa J., and Karen Alley. "INVESTIGATING THE EFFECTS OF BASAL CHANNELS ON ICE SHEET MARGIN MELTING AT PETERMANN GLACIER, GREENLAND." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321917.

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Colosio, Paolo, Marco Tedesco, and Roberto Ranzi. "Enhanced resolution mapping of surface melting over the Greenland ice sheet (1979 - 2019) from spaceborne passive microwave observations." In Proceedings of the 39th IAHR World Congress From Snow to Sea. International Association for Hydro-Environment Engineering and Research (IAHR), 2022. http://dx.doi.org/10.3850/iahr-39wc252171192022366.

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Iyer, Shivram Balasubramaniam, Sharifah Norliza Syed Salim, and Mashitah Jais. "Cost to Decarbonise." In ADIPEC. SPE, 2023. http://dx.doi.org/10.2118/216536-ms.

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Abstract Industrialization and economic growth has led to greenhouse gas emissions, primarily carbon dioxide (CO2), the major driver of climate change. As economies grow and industries expand, there may be a greater demand for energy, often met by burning fossil fuels. We are all seeing now how climate change is impacting us from rising temperatures, sea-level rise, and extreme weather events. Glaciers around the world are vanishing at an alarming rate. The disappearance of mountain glaciers is a visible manifestation of climate change. Glaciers in the Alps, Himalayas, Andes, and other mountai
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Voronovich, A. G., S. W. Abbott, P. E. Johnston, R. J. Lataitis, J. L. Leach, and R. J. Zamora. "The Greenland Ice Sheet as a Dielectric Resonator." In IGARSS 2018 - 2018 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2018. http://dx.doi.org/10.1109/igarss.2018.8519211.

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CHYLEK, PETR. "RECENT TEMPERATURE CHANGES IN GREENLAND: COASTAL STATIONS AND THE GREENLAND ICE SHEET." In International Seminar on Nuclear War and Planetary Emergencies 34th Session. WORLD SCIENTIFIC, 2006. http://dx.doi.org/10.1142/9789812773890_0015.

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Farnsworth, Lauren, Meredith A. Kelly, Yarrow Axford, et al. "LATE PLEISTOCENE AND HOLOCENE HISTORY OF THE GREENLAND ICE SHEET MARGIN, NUNATARSSUAQ, NORTHWESTERN GREENLAND." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272866.

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Reports on the topic "Greenland ice sheet melting"

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Nordhaus, William. Global Melting? The Economics of Disintegration of the Greenland Ice Sheet. National Bureau of Economic Research, 2018. http://dx.doi.org/10.3386/w24640.

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Petersen, Guðrún. Alviðruhamrar – Meteorological conditions. Icelandic Meteorological Office, 2025. https://doi.org/10.33112/damc5680.

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This report is written for EP Power Minerals ehf. that is planning activities in in SoutheastIceland. Themeteorological conditions inMýrdalssandur and Alviðruhamrar in SoutheastIceland are analysed using observations from two automatic long-term weather stations and reanalysis data from the CARRA reanalysis project. The emphasis is on the wind conditions. The climate of the region is mild and wet. There are three main wind directions, northerly, easterly and southwesterly. Winds from the north are in general dry and winds form the east wet. However, depending on the general weather conditions
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Reeh, N. Chapter 14: Dynamic and Climatic History of the Greenland Ice Sheet. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131821.

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Benson, Carl S. Stratigraphic Studies in the Snow and Firn of the Greenland Ice Sheet. Defense Technical Information Center, 1996. http://dx.doi.org/10.21236/ada337542.

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Kopera, Michal A., Francis X. Giraldo, and Wieslaw Maslowski. Ice-Sheet / Ocean Interaction Model for Greenland Fjords Using High-Order Discontinuous Galerkin Methods. Office of Scientific and Technical Information (OSTI), 2018. http://dx.doi.org/10.2172/1480068.

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