Relevant bibliographies by topics / Ice sheet modeling

Contents

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

Academic literature on the topic 'Ice sheet modeling'

Author: Grafiati
Published: 4 June 2021
Last updated: 20 February 2023

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Journal articles on the topic "Ice sheet modeling"

1

Alley, R. B., and I. Joughin. "Modeling Ice-Sheet Flow." Science 336, no. 6081 (2012): 551–52. http://dx.doi.org/10.1126/science.1220530.

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Robert, Barry L. "Modeling the Cordilleran Ice Sheet." Géographie physique et Quaternaire 45, no. 3 (2007): 287–99. http://dx.doi.org/10.7202/032876ar.

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ABSTRACT A time-dependent ice flow model is used to provide detailed reconstructions of ice growth and retreat for the southern portion of the Late Wisconsinan Cordilleran Ice Sheet. The two-dimensional, time-dependent model provides ice surface elevations and flow directions at a grid spacing of 15 km. Input to the model includes subglacial topography, a net mass balance function, and two ice flow parameters. The net mass balance function uses a polynomial equation to estimate equilibrium line altitude (ELA) across the study area. A quadratic equation is then used to provide net mass balance
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Fahrenkamp-Uppenbrink, Julia. "Modeling Antarctic ice sheet loss." Science 363, no. 6426 (2019): 495.6–496. http://dx.doi.org/10.1126/science.363.6426.495-f.

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Verbitsky, Mikhail, and Barry Saltzman. "Modeling the Antarctic ice sheet." Annals of Glaciology 25 (1997): 259–68. http://dx.doi.org/10.3189/s0260305500014130.

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A three-dimensional (3-D), high-resolution, non-linearly viscous, non-isothermal ice-sheet model is employed to calculate the “present-day” equilibrium regime of the Antarctic ice sheet and its evolution during the last glacial cycle. The model is augmented by an approximate formula for ice-sheet basal temperature, based on a scaling of the thermodynamic equation for the ice flow. Steady-state solutions for both the shape and extent of the areas of basal melting (or freezing) are shown to be in good agreement with those obtained from the solution of the full 3-D thermodynamic equation. The sol
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Verbitsky, Mikhail, and Barry Saltzman. "Modeling the Antarctic ice sheet." Annals of Glaciology 25 (1997): 259–68. http://dx.doi.org/10.1017/s0260305500014130.

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A three-dimensional (3-D), high-resolution, non-linearly viscous, non-isothermal ice-sheet model is employed to calculate the “present-day” equilibrium regime of the Antarctic ice sheet and its evolution during the last glacial cycle. The model is augmented by an approximate formula for ice-sheet basal temperature, based on a scaling of the thermodynamic equation for the ice flow. Steady-state solutions for both the shape and extent of the areas of basal melting (or freezing) are shown to be in good agreement with those obtained from the solution of the full 3-D thermodynamic equation. The sol
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Roe, Gerard H. "Modeling precipitation over ice sheets: an assessment using Greenland." Journal of Glaciology 48, no. 160 (2002): 70–80. http://dx.doi.org/10.3189/172756502781831593.

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AbstractThe interaction between ice sheets and the rest of the climate system at long time-scales is not well understood, and studies of the ice ages typically employ simplified parameterizations of the climate forcing on an ice sheet. It is important therefore to understand how an ice sheet responds to climate forcing, and whether the reduced approaches used in modeling studies are capable of providing robust and realistic answers. This work focuses on the accumulation distribution, and in particular considers what features of the accumulation pattern are necessary to model the steady-state r
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Kleman, J., J. Fastook, K. Ebert, J. Nilsson, and R. Caballero. "Pre-LGM Northern Hemisphere ice sheet topography." Climate of the Past 9, no. 5 (2013): 2365–78. http://dx.doi.org/10.5194/cp-9-2365-2013.

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Abstract. We here reconstruct the paleotopography of Northern Hemisphere ice sheets during the glacial maxima of marine isotope stages (MIS) 5b and 4.We employ a combined approach, blending geologically based reconstruction and numerical modeling, to arrive at probable ice sheet extents and topographies for each of these two time slices. For a physically based 3-D calculation based on geologically derived 2-D constraints, we use the University of Maine Ice Sheet Model (UMISM) to calculate ice sheet thickness and topography. The approach and ice sheet modeling strategy is designed to provide ro
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Robinson, A., and H. Goelzer. "The importance of insolation changes for paleo ice sheet modeling." Cryosphere 8, no. 4 (2014): 1419–28. http://dx.doi.org/10.5194/tc-8-1419-2014.

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Abstract. The growth and retreat of continental ice sheets in the past has largely been a response to changing climatic forcing. Since ablation is the principal component of mass loss for land-based ice sheets, the calculation of surface melt is an important aspect of paleo ice sheet modeling. Changes in insolation are often not accounted for in calculations of surface melt, under the assumption that the near-surface temperature transmits the majority of the climatic forcing to the ice sheet. To assess how this could affect paleo simulations, here we investigate the importance of different orb
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Koenig, S. J., A. M. Dolan, B. de Boer, et al. "Ice sheet model dependency of the simulated Greenland Ice Sheet in the mid-Pliocene." Climate of the Past 11, no. 3 (2015): 369–81. http://dx.doi.org/10.5194/cp-11-369-2015.

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Abstract. The understanding of the nature and behavior of ice sheets in past warm periods is important for constraining the potential impacts of future climate change. The Pliocene warm period (between 3.264 and 3.025 Ma) saw global temperatures similar to those projected for future climates; nevertheless, Pliocene ice locations and extents are still poorly constrained. We present results from the efforts to simulate mid-Pliocene Greenland Ice Sheets by means of the international Pliocene Ice Sheet Modeling Intercomparison Project (PLISMIP). We compare the performance of existing numerical ice
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Kleman, J., J. Fastook, K. Ebert, J. Nilsson, and R. Caballero. "Pre-LGM Northern Hemisphere paleo-ice sheet topography." Climate of the Past Discussions 9, no. 3 (2013): 2557–87. http://dx.doi.org/10.5194/cpd-9-2557-2013.

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Abstract. We here reconstruct the paleotopgraphy of Northern Hemisphere ice sheets during the glacial maxima of marine isotope stages (MIS) 5b and 4. We employ two approaches, geologically based reconstruction and numerical modeling, in mutually supportive roles to arrive at probable ice sheet extents and topographies for each of these two time slices. For a physically based 3-D calculation based on geologically derived 2-D constraints, we use the University of Maine Ice Sheet Model (UMISM) to calculate ice-sheet thickness and topography. The approach and ice-sheet modeling strategy is designe
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Dissertations / Theses on the topic "Ice sheet modeling"

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Gomez, Natalya Alissa. "On Sea Level - Ice Sheet Interactions." Thesis, Harvard University, 2013. http://dissertations.umi.com/gsas.harvard:11242.

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This thesis focuses on the physics of static sea-level changes following variations in the distribution of grounded ice and the influence of these changes on the stability and dynamics of marine ice sheets. Gravitational, deformational and rotational effects associated with changes in grounded ice mass lead to markedly non-uniform spatial patterns of sea-level change. I outline a revised theory for computing post-glacial sea-level predictions and discuss the dominant physical effects that contribute to the patterns of sea-level change associated with surface loading on different timescales.
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Holmgren, Hanna. "Computational Ice Dynamics and Hydraulics : Towards a Coupling in the Ice Sheet Code ARCTIC-TARAH." Thesis, Uppsala universitet, Institutionen för informationsteknologi, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-179861.

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Numerical ice sheet modeling is a rather young discipline: it started in the 1950s. The "first generation" models developed at that time are currently being replaced by "new generations" ones, such as e.g. ARCTIC-TARAH. ARCTIC-TARAH is a Bert Bolin Center for Climate Research spin-off from the Pennsylvania State University Ice sheet model (PSUI). When the Bolin Center received PSUI for subsequent independent development and adaption of the code to Arctic settings in 2010, an initial inspection of the source code suggested that PSUI also contained a module that allows for the treatment of glaci
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Ahlkrona, Josefin. "Implementing Higher Order Dynamics into the Ice Sheet Model SICOPOLIS." Thesis, Uppsala universitet, Avdelningen för teknisk databehandling, 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-146947.

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Ice sheet modeling is an important tool both for reconstructing past ice sheets and predicting their future evolution, but is complex and computationally costly. It involves modeling a system including the ice sheet, ice shelves and ice streams, which all have different dynamical behavior. The governing equations are non-linear, and to capture a full glacial cycle more than 100,000 years need to be simulated. To reduce the problem size, approximations of the equations are introduced. The most common approximation, the Shallow Ice Approximation (SIA), works well in the ice bulk but fails in e.g
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Jonsson, Eskil. "Ice Sheet Modeling: Accuracy of First-Order Stokes Model with Basal Sliding." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-360245.

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Some climate models are still lacking features such as dynamical modelling of ice sheets due to their computational cost which results in poor accuracy and estimates of e.g. sea level rise. The need for low-cost high-order models initiated the development of the First-Order Stokes (or Blatter-Pattyn) model which retains much of the accuracy of the full-Stokes model but is also cost-effective. This model has proven accurate for ice sheets and glaciers with frozen bedrocks, or no-slip basal boundary conditions. However, experimental evidence seems to be lacking regarding its accuracy under slidi
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Lande, Daniel Ross. "Implementation of an XML-based user interface with applications in ice sheet modeling." The University of Montana, 2009. http://etd.lib.umt.edu/theses/available/etd-12152008-222224/.

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The scientific domain presents unique challenges to software developers. This thesis describes the application of design patterns to the problem of dynamically changing interfaces to scientific application software (GLIMMER, which performs ice sheet modeling). In its present form, GLIMMER uses a text configuration file to define model behavior, set parameters, and structure model input/output (I/O). The creation of the configuration file presents a significant problem to users due to its format and complexity. GLIMMER is still under development, and the number of changes to configuration param
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Docquier, David. "Representing grounding-line dynamics in Antarctic ice-sheet models." Doctoral thesis, Universite Libre de Bruxelles, 2013. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/209400.

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Since the mid-20th century, global average temperatures have dramatically risen mostly due to the increasing amount of greenhouse gas emissions in the atmosphere. The effects of this recent global warming are already evident and could be exacerbated in the near future if no real action is taken. Recent ice loss in West Antarctica, monitored by satellite measurements and other techniques, gives cause for concern in such a warming world. A major part of this loss has been driven by warm water masses penetrating underneath the ice shelves in this region. This has led to a flow acceleration of the
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Robinson, Alexander. "Modeling the Greenland Ice Sheet response to climate change in the past and future." Phd thesis, Universität Potsdam, 2011. http://opus.kobv.de/ubp/volltexte/2011/5043/.

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The Greenland Ice Sheet (GIS) contains enough water volume to raise global sea level by over 7 meters. It is a relic of past glacial climates that could be strongly affected by a warming world. Several studies have been performed to investigate the sensitivity of the ice sheet to changes in climate, but large uncertainties in its long-term response still exist. In this thesis, a new approach has been developed and applied to modeling the GIS response to climate change. The advantages compared to previous approaches are (i) that it can be applied over a wide range of climatic scenarios (both in
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Muschitiello, Francesco. "Deglacial impact of the Scandinavian Ice Sheet on the North Atlantic climate system." Doctoral thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-128147.

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The long warming transition from the Last Ice Age into the present Interglacial period, the last deglaciation, holds the key to our understanding of future abrupt climate change. In the last decades, a great effort has been put into deciphering the linkage between freshwater fluxes from melting ice sheets and rapid shifts in global ocean-atmospheric circulation that characterized this puzzling climate period. In particular, the regional expressions of climate change in response to freshwater forcing are still largely unresolved. This projects aims at evaluating the environmental, hydro-climati
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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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Colleoni, Florence. "On the Late Saalian glaciation : A climate modeling study." Doctoral thesis, Stockholms universitet, Institutionen för geologi och geokemi, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-29284.

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This thesis focuses on the glaciation of the Late Saalian period (160 -140 ka) over Eurasia. The Quaternary Environment of the Eurasian North (QUEEN) project determined that during this period, the Eurasian ice sheet was substantially larger than during the entire Weichselian cycle and especially that of the Last Glacial Maximum (21 ka, LGM). The Late Saalian astronomical forcing was different than during the LGM while greenhouse gas concentrations were similar. To understand how this ice sheet could have grown so large over Eurasia during the Late Saalian, we use an Atmospherical General Circ
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Books on the topic "Ice sheet modeling"

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Hughes, Terence J. Holistic ice sheet modeling: A first-order approach. Nova Science Publishers, 2011.

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Staroszczyk, Ryszard. Constitutive modelling of creep induced anisotropy of ice. Institute of Hydro-Engineering of the Polish Academy of Sciences, 2004.

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Huybrechts, Philippe. The Antarctic ice sheet and environmental change: A three-dimensional modelling study = Der antarktische Eisschild und globale Umweltveränderungen : eine dreidimensionale Modellstudie. Alfred Wegener Institute for Polar and Marine Research, 1992.

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Abe-Ouchi, Ayako. Ice sheet response to climate changes: A modelling approach. Geographisches Institut ETH, 1993.

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Mayer, Christoph. Numerische Modellierung der Übergangszone zwischen Eisschild und Schelfeis =: Numerical modelling of the transition zone between an ice sheet and an ice shelf. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1996.

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International Symposium on Ice Sheet Modelling (1995 Chamonix, France). Papers from the International Symposium on Ice Sheet Modelling held in Chamonix, France, 18-22 September 1995. International Glaciological Society, 1996.

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MacAyeal, D. R. Changes in glaciers and ice sheets: Observations, modelling and environmental interactions. Edited by International Glaciological Society. International Glaciological Society, 2014.

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Greuell, Wouter. Numerical modelling of the energy balance and the Englacial temperature at the ETH camp, West Greenland. Geographisches Institut, Eidgenössische Technische Hochschule Zürich, 1992.

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Kolumban, Hutter, and International Glaciological Society, eds. Papers from the EISMINT/EPICA Symposium on Ice Sheet Modelling and Deep Ice Drilling : Den Haag, The Netherlands, 21-22 April, 1999. International Glaciological Society, 2000.

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International, Symposium on Physical and Mechanical Processes in Ice in Relation to Glacier and Ice-sheet Modelling (2002 Chamonix-Mont-Blanc France). Papers from the International Symposium on Physical and Mechanical Processes in Ice in Relation to Glacier and Ice-sheet Modelling: Held in Chamonix, France, 25-30 August 2002. International Glaciological Society, 2003.

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Book chapters on the topic "Ice sheet modeling"

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Lliboutry, Louis A. "Ice Sheet Dynamics." In Flow and Creep in the Solar System: Observations, Modeling and Theory. Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-015-8206-3_24.

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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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Letréguilly, Anne, and Catherine Ritz. "Modelling of the Fennoscandian Ice Sheet." In Ice in the Climate System. Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-85016-5_2.

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Budd, W. F., and P. Rayner. "Modelling Ice Sheet and Climate Changes through the Ice Ages." In Ice in the Climate System. Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-85016-5_18.

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Budd, W. F., B. J. McInnes, D. Jenssen, and I. N. Smith. "Modelling the Response of the West Antarctic Ice Sheet to a Climatic Warming." In Dynamics of the West Antarctic Ice Sheet. Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3745-1_17.

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Budd, W. F., and D. Jenssen. "Numerical Modelling of the Large-Scale Basal Water Flux under the West Antarctic Ice Sheet." In Dynamics of the West Antarctic Ice Sheet. Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3745-1_16.

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Hulbe, C. L., and A. J. Payne. "The Contribution of Numerical Modelling to Our Understanding of the West Antarctic Ice Sheet." In The West Antarctic Ice Sheet: Behavior and Environment. American Geophysical Union, 2013. http://dx.doi.org/10.1029/ar077p0201.

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Fowler, Andrew C. "Modelling the Flow of Glaciers and Ice Sheets." In Continuum Mechanics and Applications in Geophysics and the Environment. Springer Berlin Heidelberg, 2001. http://dx.doi.org/10.1007/978-3-662-04439-1_12.

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Bueler, Ed. "Numerical Modelling of Ice Sheets, Streams, and Shelves." In Springer Textbooks in Earth Sciences, Geography and Environment. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-42584-5_8.

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Bamber, Jonathan L. "Modelling Ice Sheet Dynamics with the Aid of Satellite-Derived Topography." In Spatial Modelling of the Terrestrial Environment. John Wiley & Sons, Ltd, 2005. http://dx.doi.org/10.1002/0470094001.ch2.

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Conference papers on the topic "Ice sheet modeling"

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Ka¨rna¨, Tuomo, Yan Qu, and Walter L. Ku¨hnlein. "A New Spectral Method for Modeling Dynamic Ice Actions." In ASME 2004 23rd International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2004. http://dx.doi.org/10.1115/omae2004-51360.

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This paper presents a method of evaluating the response of a vertical offshore structure that is subjected to dynamic ice actions. The model concerns a loading scenario where a uniform ice sheet is drifting and crushing against the structure. Full scale data obtained at the lighthouse Norstro¨msgrund is used in the derivation of a method that applies both to narrow and wide structures. A large amount of events with directly measured local forces was used to derive formulas for spectral density functions of the ice force. A non-dimensional formula that was derived for the autospectrum applies f
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Sok, Ratnak, and Jin Kusaka. "Thermoelectric Exhaust Heat Recovery to Maximize Brake Thermal Efficiency of Advanced Diesel Engines: Modeling and Baseline Analysis." In ASME 2022 ICE Forward Conference. American Society of Mechanical Engineers, 2022. http://dx.doi.org/10.1115/icef2022-90505.

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Abstract This work demonstrates the enhancement of brake thermal efficiency (BTE) of an advanced, turbocharged, production-intent 2.2 L diesel engine with a thermoelectric waste heat recovery system (TEG-WHR). The integrated engine model with the TEG is developed using 0D/1D software. Experimental data from the corrugated fin TEG under fin pitch = 1.0–2.0 mm, inlet gas temperatures (200–300 °C), and mass flow rates (5.0–15.0 g/s) are used for validating the model. The TEG model can reproduce measured pressure drop, heat transfer, and thermal performance characteristics. A 1-cylinder engine mod
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Xu, Ning, and Qianjin Yue. "Dynamic Ice Forces Analysis of Conical Structure Based on Direct Measurement." In ASME 2010 29th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2010. http://dx.doi.org/10.1115/omae2010-20245.

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The dynamic ice force is produced by failure process during ice interaction with structure. The best way for describing and modeling this process is using directly measured ice force on full scale structure in situ. In this paper, the ice force variation and corresponded failure process of ice sheet were recorded by ice load panel and video camera. It is demonstrated that when ice acting on upward narrow cone and in bending failure and well clearing by side of the cone. The form of ice force history looks like impulse signal.
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Pohl, Alexandre, Yannick Donnadieu, Yannick Donnadieu, et al. "MODELING ORDOVICIAN ICE SHEET AND THE SEA-LEVEL FINGERPRINT OF ITS COLLAPSE: TOWARD A CONSISTENT PICTURE OF THE ORDOVICIAN GLACIATION." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-352774.

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Dickens, Phillip M., Christopher Dufour, and James Fastook. "The Scalability of Embedded Structured Grids and Unstructured Grids in Large Scale Ice Sheet Modeling on Distributed Memory Parallel Computers." In 2018 IEEE International Parallel and Distributed Processing Symposium Workshops (IPDPSW). IEEE, 2018. http://dx.doi.org/10.1109/ipdpsw.2018.00152.

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Zhang, Yuxi, and Bingbin Yu. "An Ice-Structure Interaction Model Using Fourier Series for Offshore Wind Tower Analysis." In ASME 2018 1st International Offshore Wind Technical Conference. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/iowtc2018-1074.

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Intermittent brittle crushing often occurs in the movement of an ice sheet against an offshore structure. Matlock’s ice-structure interaction model is used to simulate the behavior of the ice crushing by modeling ice teeth indentation contacting a spring-mass-dashpot structure. The dynamic behavior of this analytical ice-structure interaction system is studied using Fourier analysis to efficiently predict the response amplitude of specific dynamic periodicity at a given indentation speed. The system’s equations of motion are established based on the assumption of continuous ice indentation. Th
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Perego, Mauro. "Advances in Modeling the Thermo-Mechanical state of Ice Sheets." In Proposed for presentation at the Coupled Problems 2021. US DOE, 2021. http://dx.doi.org/10.2172/1873266.

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Tarasov, Lev, Taimaz Bahadory, and Marilena Sophie Geng. "THE RELATIONSHIP BETWEEN TERRESTRIAL ICE SHEET MARGINS AND MEAN SUMMER TEMPERATURE FROM FULLY COUPLED ICE AND CLIMATE MODELLING." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358330.

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Kurukuri, Srihari, and Michael Worswick. "Modeling of Strength Differential Effects in HCP Sheet Materials." In ASME 2014 International Manufacturing Science and Engineering Conference collocated with the JSME 2014 International Conference on Materials and Processing and the 42nd North American Manufacturing Research Conference. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/msec2014-4134.

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A simple approach is proposed to employ symmetric yield functions for modeling the tension-compression asymmetry commonly observed in hcp materials. In this work, the strength differential (SD) effect is modeled by choosing separate symmetric plane stress Barlat Yld 2000 yield functions for the tension i.e., in the first quadrant of principal stress space, and compression i.e., third quadrant of principal stress space. In the second and fourth quadrants, the yield locus is constructed by adopting Bézier interpolating functions between uniaxial tensile and compressive stress states. The main ad
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Benhamou, Sidi Mohamed, Mohammed Hamouni, and Antonio Jose Lozano Guerrero. "Modeling of electromagnetic shielding properties of conductive sheet using the matrix formalism." In 2015 4th International Conference on Electrical Engineering (ICEE). IEEE, 2015. http://dx.doi.org/10.1109/intee.2015.7416704.

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Reports on the topic "Ice sheet modeling"

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Hughes, T. J., and J. L. Fastook. Global ice sheet modeling. Office of Scientific and Technical Information (OSTI), 1994. http://dx.doi.org/10.2172/145218.

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Ghattas, Omar. Uncertainty Quantification for Large-Scale Ice Sheet Modeling. Office of Scientific and Technical Information (OSTI), 2016. http://dx.doi.org/10.2172/1237006.

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Asay-Davis, Xylar Storm. Final Report: Modeling coupled ice sheet-ocean interactions in the Model for Prediction Across Scales (MPAS) and in DOE Earth System Models. Office of Scientific and Technical Information (OSTI), 2019. http://dx.doi.org/10.2172/1490084.

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Waisman, Haim, and Ray Tuminaro. Modeling the Fracture of Ice Sheets on Parallel Computers. Office of Scientific and Technical Information (OSTI), 2013. http://dx.doi.org/10.2172/1127195.

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Modlo, Yevhenii O., Serhiy O. Semerikov, Ruslan P. Shajda, Stanislav T. Tolmachev, and Oksana M. Markova. Methods of using mobile Internet devices in the formation of the general professional component of bachelor in electromechanics competency in modeling of technical objects. [б. в.], 2020. http://dx.doi.org/10.31812/123456789/3878.

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The article describes the components of methods of using mobile Internet devices in the formation of the general professional component of bachelor in electromechanics competency in modeling of technical objects: using various methods of representing models; solving professional problems using ICT; competence in electric machines and critical thinking. On the content of learning academic disciplines “Higher mathematics”, “Automatic control theory”, “Modeling of electromechanical systems”, “Electrical machines” features of use are disclosed for Scilab, SageCell, Google Sheets, Xcos on Cloud in
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Modlo, Yevhenii O., Serhiy O. Semerikov, Pavlo P. Nechypurenko, Stanislav L. Bondarevskyi, Olena M. Bondarevska, and Stanislav T. Tolmachev. The use of mobile Internet devices in the formation of ICT component of bachelors in electromechanics competency in modeling of technical objects. [б. в.], 2019. http://dx.doi.org/10.31812/123456789/3264.

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Computer simulation of technical objects and processes is one of the components of the system of professional training of a modern electromechanics engineer. It has been established that despite the fact that mobile Internet devices (MID) are actively used by electrical engineers, the methods of using them in the process of bachelor in electromechanics training is considered only in some domestic scientific studies. The article highlights the components of the methods of using MID in the formation of the ICT component of the competence of the bachelor in electromechanics in modeling of technic
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Otto-Bliesner, Bette, William Lipscomb, Shawn Marshall, et al. Modeling Long-Term Changes in Climate, Ice Sheets and Sea Level: Using the Paleo Record to Understand Possibilities for the Future. Office of Scientific and Technical Information (OSTI), 2014. http://dx.doi.org/10.2172/1714361.

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