Auswahl der wissenschaftlichen Literatur zum Thema „Marine Ice sheet“
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Zeitschriftenartikel zum Thema "Marine Ice sheet"
Gandy, Niall, Lauren J. Gregoire, Jeremy C. Ely, Christopher D. Clark, David M. Hodgson, Victoria Lee, Tom Bradwell und Ruza F. Ivanovic. „Marine ice sheet instability and ice shelf buttressing of the Minch Ice Stream, northwest Scotland“. Cryosphere 12, Nr. 11 (23.11.2018): 3635–51. http://dx.doi.org/10.5194/tc-12-3635-2018.
Der volle Inhalt der QuelleMulder, T. E., S. Baars, F. W. Wubs und H. A. Dijkstra. „Stochastic marine ice sheet variability“. Journal of Fluid Mechanics 843 (23.03.2018): 748–77. http://dx.doi.org/10.1017/jfm.2018.148.
Der volle Inhalt der QuelleHASELOFF, MARIANNE, und OLGA V. SERGIENKO. „The effect of buttressing on grounding line dynamics“. Journal of Glaciology 64, Nr. 245 (07.05.2018): 417–31. http://dx.doi.org/10.1017/jog.2018.30.
Der volle Inhalt der QuelleSchoof, Christian. „Marine ice sheet stability“. Journal of Fluid Mechanics 698 (15.03.2012): 62–72. http://dx.doi.org/10.1017/jfm.2012.43.
Der volle Inhalt der QuellePegler, Samuel S. „Suppression of marine ice sheet instability“. Journal of Fluid Mechanics 857 (25.10.2018): 648–80. http://dx.doi.org/10.1017/jfm.2018.742.
Der volle Inhalt der QuellePegler, Samuel S. „Marine ice sheet dynamics: the impacts of ice-shelf buttressing“. Journal of Fluid Mechanics 857 (25.10.2018): 605–47. http://dx.doi.org/10.1017/jfm.2018.741.
Der volle Inhalt der QuelleMeur, E. Le, und Richard C. A. Hindmarsh. „Coupled marine-ice-sheet/Earth dynamics using a dynamically consistent ice-sheet model and a self-gravitating viscous Earth model“. Journal of Glaciology 47, Nr. 157 (2001): 258–70. http://dx.doi.org/10.3189/172756501781832322.
Der volle Inhalt der QuelleLeguy, Gunter R., William H. Lipscomb und Xylar S. Asay-Davis. „Marine ice sheet experiments with the Community Ice Sheet Model“. Cryosphere 15, Nr. 7 (14.07.2021): 3229–53. http://dx.doi.org/10.5194/tc-15-3229-2021.
Der volle Inhalt der QuelleTsai, Victor C., Andrew L. Stewart und Andrew F. Thompson. „Marine ice-sheet profiles and stability under Coulomb basal conditions“. Journal of Glaciology 61, Nr. 226 (2015): 205–15. http://dx.doi.org/10.3189/2015jog14j221.
Der volle Inhalt der QuelleZweck, Chris, und Philippe Huybrechts. „Modeling the marine extent of Northern Hemisphere ice sheets during the last glacial cycle“. Annals of Glaciology 37 (2003): 173–80. http://dx.doi.org/10.3189/172756403781815870.
Der volle Inhalt der QuelleDissertationen zum Thema "Marine Ice sheet"
Koester, Alexandria Jo. „Rapid thinning of the Laurentide Ice Sheet in coastal Maine, USA during late Heinrich Stadial 1:“. Thesis, Boston College, 2017. http://hdl.handle.net/2345/bc-ir:107308.
Der volle Inhalt der QuelleFew data are available to infer the thinning rate of the Laurentide Ice Sheet (LIS) through the last deglaciation, despite its importance for constraining past ice sheet response to climate warming. We measured 31 cosmogenic 10Be exposure ages in samples collected on coastal mountainsides in Acadia National Park and from the slightly inland Pineo Ridge moraine complex, a ~100-km-long glaciomarine delta, to constrain the timing and rate of LIS thinning and subsequent retreat in coastal Maine. Samples collected along vertical transects in Acadia National Park have indistinguishable exposure ages over a 300 m range of elevation, suggesting that rapid, century-scale thinning occurred at 15.2 ± 0.7 ka, similar to the timing of abrupt thinning inferred from cosmogenic exposure ages at Mt. Katahdin in central Maine (Davis et al., 2015). This rapid ice sheet surface lowering, which likely occurred during the latter part of the cold Heinrich Stadial 1 event (19-14.6 ka), may have been due to enhanced ice-shelf melt and calving in the Gulf of Maine, perhaps related to regional oceanic warming associated with a weakened Atlantic Meridional Overturning Circulation at this time. The ice margin subsequently stabilized at the Pineo Ridge moraine complex until 14.5 ± 0.7 ka, near the onset of Bølling Interstadial warming. Our 10Be ages are substantially younger than marine radiocarbon constraints on LIS retreat in the coastal lowlands, suggesting that the deglacial marine reservoir effect in this area was ~1,200 14C years, perhaps also related to the sluggish Atlantic Meridional Overturning Circulation during Heinrich Stadial 1
Thesis (MS) — Boston College, 2017
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Earth and Environmental Sciences
Nicholl, Joseph Anthony Leo. „Changes in ice sheet dynamics across the mid-Pleistocene transition recorded in North Atlantic sediments“. Thesis, University of Cambridge, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648858.
Der volle Inhalt der QuelleSimmons, Sarah-Louise. „An investigation into the effect of glacially exported nutrients from the Greenland Ice Sheet on marine primary production“. Thesis, University of Bristol, 2016. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.742982.
Der volle Inhalt der QuelleCook, Carys Patricia. „Insights into the behaviour of the Pliocene East Antarctic ice sheet from provenance studies of marine sediments using radiogenic isotopoes“. Thesis, Imperial College London, 2013. http://hdl.handle.net/10044/1/14262.
Der volle Inhalt der QuelleSacchetti, Fabio. „Late Quaternary sedimentation associated with the British-Irish Ice Sheet on the NW Irish continental slope: a marine geological and geophysical investigation“. Thesis, University of Manchester, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.646396.
Der volle Inhalt der QuelleLeigh, Sasha Naomi Bharier. „A study of the dynamics of the British Ice Sheet during Marine Isotope Stages 2 and 3, focusing on Heinrich Events 2 and 4 and their relationship to the North Atlantic glaciological and climatological conditions /“. St Andrews, 2007. http://hdl.handle.net/10023/525.
Der volle Inhalt der QuelleHibbert, Fiona Danielle. „Dynamics of the British Ice Sheet and prevailing hydrographic conditions for the last 175,000 years : an investigation of marine sediment core MD04-2822 from the Rockall Trough“. Thesis, University of St Andrews, 2011. http://hdl.handle.net/10023/3136.
Der volle Inhalt der QuelleHill, Heather W. „Abrupt climate change during the last glacial period : a Gulf of Mexico perspective“. [Tampa, Fla] : University of South Florida, 2006. http://purl.fcla.edu/usf/dc/et/SFE0001539.
Der volle Inhalt der QuelleVan, Aalderen Victor. „Modéliser l'évolution du climat global et de la calotte eurasienne pendant la dernière déglaciation“. Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ029.
Der volle Inhalt der QuelleThe marine West Antarctic ice sheet is characterized by being largely in contact with the ocean. The latest observations reveal an acceleration in its mass loss over the last few decades, mainly due to increased melting under floating ice shelves. However, its future evolution remains highly uncertain, due to our poor understanding of the physical processes at play between the ice sheet and the ocean.The last deglaciation (21 ka-11 ka) is one of the most recent major climatic changes in our history. This period is marked by an increase in global atmospheric temperatures and the melting of the North American and Eurasian ice sheets. The study of the Barents-Kara Ice Sheet (BKIS), which covered the Barents and Kara Seas during the Last Glacial Maximum (LGM, 21 ka) and was an integral part of the Eurasian Ice Sheet, is of particular interest because of its common features with present-day West Antarctica. Identifying the mechanisms responsible for its retreat allows to provide information to better understand the West Antarctic behavior within under present and future climatic conditions.The impact of climate on the evolution of a marine ice sheet depends on two main processes: The surface mass balance, depending on atmospheric temperatures and precipitation, and melting under floating ice, related to oceanic temperatures and salinity. In order to identify the mechanisms triggering the BKIS retreat, I used the GRISLI2.0 ice-sheet model to analyse the ice-sheet response to climate perturbations at the LGM. This study highlighted the key role of atmospheric temperatures in triggering the melting of the ice sheet via surface melting, while ocean temperatures had only a limited impact despite a large part of BKIS being in contact with the ocean. I also identified that the total retreat of BKIS could be attributed to a mechanical instability at the grounding line, caused by a decrease in ice thickness resulting from an increase in surface melting.In order to better understand the impact of ice sheets on the global climate, I have also carried out the first transient simulation of the last deglaciation with the IPSL-CM5A2 model, modifying the geometry of the ice sheets provided by the GLAC-1D reconstruction at some key periods. The simulations show a warming trend in line with the reconstructions, particularly during MWP1A, which was characterised by an abrupt rise in atmospheric temperatures. Using sensitivity experiments, I have shown that changes in the ice sheet geometry have contributed to the increase in atmospheric temperatures via temperature-altitude feedbacks and the albedo effect. Moreover, I have shown that ocean dynamics have been significantly altered by freshwater fluxes from the melting ice sheets. This has led to a weakening of the strength of the Atlantic Meridional Overturning Circulation and a reduction of its deepening, resulting in a warming slowdown, mainly located in the North Atlantic Ocean. In addition, the IPSL-CM5A2 experiments all simulate a shutdown of the Antarctic bottom water circulation at the onset of MWP1A, leading to a significant cooling of about 100 years in the Amundsen Sea, followed by a restart of this circulation.This work is contributing to a better understanding of the complex mechanisms governing the dynamics of the ice sheets and their interaction with the climate, while also providing a basis for anticipating the consequences of current and future climate change, particularly in West Antarctica
Nowicki, Sophie Marie Jeanne. „Modelling the transition zone of marine ice sheets“. Thesis, University College London (University of London), 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.499076.
Der volle Inhalt der QuelleBücher zum Thema "Marine Ice sheet"
Bindschadler, R. A. SeaRISE: A multidisciplinary research initiative to predict rapid changes in global sea level caused by collapse of marine ice sheets. Washington, D.C: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Division, 1990.
Den vollen Inhalt der Quelle findenOffice, General Accounting. Coast Guard: Federal costs resulting from the Exxon Valdez oil spill : fact sheet for congressional requesters. Washington, D.C: GAO, 1990.
Den vollen Inhalt der Quelle findenKassens, Heidemarie. Sistema mori͡a Laptevykh i prilegai͡ushchikh moreĭ Arktiki: Sovremennoe sostoi͡anie i istorii͡a razvitii͡a. Moskva: Moskovskiĭ gos. universitet, 2009.
Den vollen Inhalt der Quelle findenBindschadler, R. A. SeaRISE: a multidisciplinary research initiative to predict rapid changes in global sea level caused by collapse of marine ice sheets: Proceedings of a workshop cosponsored by the National Science Foundation, Washington, D.C., and the National Aeronautics and Space Administration, Washington, D.C., and held in College Park, Maryland, January 23-25, 1990. Greenbelt, Md: Goddard Space Flight Center, 1990.
Den vollen Inhalt der Quelle findenOmstedt, Anders. The Development of Climate Science of the Baltic Sea Region. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.654.
Der volle Inhalt der QuelleBuchteile zum Thema "Marine Ice sheet"
Kumar, Rajesh. „Marine Ice Sheet“. In Encyclopedia of Earth Sciences Series, 725. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_340.
Der volle Inhalt der QuelleMulder, T. E., H. A. Dijkstra und F. W. Wubs. „Numerical Bifurcation Analysis of Marine Ice Sheet Models“. In Computational Methods in Applied Sciences, 503–27. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91494-7_14.
Der volle Inhalt der QuellePattyn, Frank, Ann Huyghe, Sang De Brabander und Bert De Smedt. „Role of Transition Zones in Marine Ice Sheet Dynamics“. In Collected Reprint Series, 1–10. Washington, DC: American Geophysical Union, 2014. http://dx.doi.org/10.1002/9781118782033.ch20.
Der volle Inhalt der QuelleScherer, Reed P. „Quaternary interglacials and the West Antarctic Ice Sheet“. In Earth's Climate and Orbital Eccentricity: The Marine Isotope Stage 11 Question, 103–12. Washington, D. C.: American Geophysical Union, 2003. http://dx.doi.org/10.1029/137gm08.
Der volle Inhalt der QuellePollard, David, und Robert M. Deconto. „A Coupled Ice-Sheet/Ice-Shelf/Sediment Model Applied to a Marine-Margin Flowline: Forced and Unforced Variations“. In Glacial Sedimentary Processes and Products, 37–52. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304435.ch4.
Der volle Inhalt der QuelleSingh, Ashutosh K., Devesh K. Sinha, Vikram Pratap Singh, Kirtiranjan Mallick, Ankush Shrivastava und Tushar Kaushik. „Cenozoic Evolution of Antarctic Ice Sheet, Circum Antarctic Circulation and Antarctic Climate: Evidence from Marine Sedimentary Records“. In Earth and Environmental Sciences Library, 47–71. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-87078-2_4.
Der volle Inhalt der QuelleHindmarsh, Richard C. A. „Qualitative Dynamics of Marine Ice Sheets“. In Ice in the Climate System, 67–99. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-85016-5_5.
Der volle Inhalt der QuelleJohnston, Arch C. „The Effect of Large Ice Sheets on Earthquake Genesis“. In Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound, 581–99. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2311-9_34.
Der volle Inhalt der QuelleHolmes, R., J. Bulat, I. Hamilton und D. Long. „Morphology of an Ice-Sheet Limit and Constructional Glacially-Fed Slope Front, Faroe-Shetland Channel“. In European Margin Sediment Dynamics, 149–52. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-55846-7_24.
Der volle Inhalt der QuelleGrgić, Marijan, und Tomislav Bašić. „Radar Satellite Altimetry in Geodesy - Theory, Applications and Recent Developments“. In Geodetic Sciences - Theory, Applications and Recent Developments [Working Title]. IntechOpen, 2021. http://dx.doi.org/10.5772/intechopen.97349.
Der volle Inhalt der QuelleKonferenzberichte zum Thema "Marine Ice sheet"
Dowdeswell, Julian A. „THE GEOMORPHIC SIGNATURE OF PAST ICE-SHEET GROUNDING LINES IN THE MARINE RECORD“. In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306091.
Der volle Inhalt der QuelleShakun, Jeremy D., Lee B. Corbett, Paul R. Bierman und Susan H. Zimmerman. „PLIOCENE GREENLAND ICE SHEET GROWTH RECORDED BY IN SITU 10BE DECREASE IN MULTIPLE MARINE SEDIMENT CORES“. In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305299.
Der volle Inhalt der QuelleHemming, Sidney. „MARINE SEDIMENT PROVENANCE EVIDENCE FOR THE EXTENT OF THE LAURENTIDE ICE SHEET DURING THE LAST GLACIAL CYCLE“. In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-379913.
Der volle Inhalt der QuelleDalton, April S., Tamara Pico, Evan J. Gowan, John J. Clague, Steven Forman, Isabelle McMartin, Perrti Sarala und Karin F. Helmens. „REVIEWING GEOLOGICAL AND NUMERICAL EVIDENCE ON THE EXTENT OF THE LAURENTIDE ICE SHEET DURING MARINE ISOTOPE STAGE 3“. In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380966.
Der volle Inhalt der QuelleChrist, Andrew J., und David R. Marchant. „A TERRESTRIAL PERSPECTIVE OF THE LGM IN MCMURDO SOUND, ANTARCTICA: IMPLICATIONS FOR MARINE ICE SHEET DYNAMICS, ICE FLOW, AND DEGLACIATION OF THE ROSS SEA EMBAYMENT“. In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305311.
Der volle Inhalt der QuelleParker, Shane T., und Jonathan P. Warnock. „THE EFFECT OF A WESTERN ANTARCTIC ICE SHEET COLLAPSE ON NUTRIENT RECYCLING RATES DURING MARINE ISOTOPE STAGE 31: INITIAL FINDINGS“. In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-311175.
Der volle Inhalt der QuelleVenturelli, Ryan, Brad Rosenheim, Christina Davis, Alex Michaud, Brenna Boehman, Brent Christner, Valier Galy et al. „Millennial scale marine incursion into an isolated environment fuels a contemporary subglacial microbial community beneath the West Antarctic Ice Sheet“. In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.13607.
Der volle Inhalt der QuelleLarson, Phillip, Howard D. Mooers, Angela J. Berthold und Kristi M. Kotrapu. „SEDIMENT TRANSPORT CYCLES OF THE LAURENTIDE ICE SHEET I: SOFT TO HARD BED TRANSITION DURING WISCONSIN MARINE ISOTOPE STAGE 5D-2“. In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-348205.
Der volle Inhalt der QuelleBANIK, ARNOB, M. H. KHAN und K. T. TAN. „IMPACT PERFORMANCE COMPARISON OF FIBER REINFORCED COMPOSITE SANDWICH STRUCTURES IN ARCTIC CONDITION“. In Proceedings for the American Society for Composites-Thirty Seventh Technical Conference. Destech Publications, Inc., 2022. http://dx.doi.org/10.12783/asc37/36380.
Der volle Inhalt der QuelleDegnan, John J., und Steven C. Cohen. „Spaceborne picosecond lidars for geoscience and other remote sensing applications“. In OSA Annual Meeting. Washington, D.C.: Optica Publishing Group, 1986. http://dx.doi.org/10.1364/oam.1986.thk2.
Der volle Inhalt der QuelleBerichte der Organisationen zum Thema "Marine Ice sheet"
Kerr, D. E. Reconnaissance surficial geology, Brichta Lake, Nunavut, NTS 76-P. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329670.
Der volle Inhalt der QuellePaulen, R. C., J. M. Rice und M. Ross. Surficial geology, Lac aux Goélands, Quebec, NTS 23-P southeast. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328291.
Der volle Inhalt der QuelleTremblay, T., und M. Lamothe. New contributions to the ice-flow chronology in the Boothia-Lancaster Ice Stream catchment area. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331062.
Der volle Inhalt der QuelleTremblay, T., und M. Lamothe. New contributions to the ice-flow chronology in the Boothia-Lancaster ice-stream catchment area, Nunavut. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331424.
Der volle Inhalt der QuelleSmith, I. R. Surficial geology, La Biche River northwest, Yukon-Northwest Territories, NTS 95-C/11, 12, 13, and 14. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330591.
Der volle Inhalt der QuelleKerr, D. E. Reconnaissance surficial geology, Nose Lake, Nunavut-Northwest Territories, NTS 76-F. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329666.
Der volle Inhalt der QuelleBartolino, Valerio, Birgit Koehler und Lena Bergström, Hrsg. Climate effects on fish in Sweden : Species-Climate Information Sheets for 32 key taxa in marine and coastal waters. Department of Aquatic Resources, Swedish University of Agricultural Sciences, 2023. http://dx.doi.org/10.54612/a.4lmlt1tq5j.
Der volle Inhalt der QuelleSurficial geology, Dendale Lake, Yukon-Northwest Territories, NTS 95-C/15. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331886.
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