Shear margins in upper half of Northeast Greenland Ice Stream were established two millennia ago
暂无分享,去创建一个
P. Bons | D. Dahl-Jensen | N. Neckel | F. Wilhelms | Nicolas Stoll | J. Eichler | I. Weikusat | S. Franke | J. Kerch | Tamara de Riese | T. Sachau | Yuanbang Hu | M. Llorens | H. Miller | J. Paden | T. Binder | D. Jansen | Catherine C. Bauer | O. Eisen | Yu Zhang
[1] O. Eisen,et al. Three-dimensional topology dataset of folded radar stratigraphy in northern Greenland , 2023, Scientific data.
[2] O. Eisen,et al. Crystal orientation fabric anisotropy causes directional hardening of the Northeast Greenland Ice Stream , 2023, Nature communications.
[3] O. Eisen,et al. Holocene ice-stream shutdown and drainage basin reconfiguration in northeast Greenland , 2022, Nature Geoscience.
[4] P. Bons,et al. Comment on “Exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream” by Smith-Johnsen et al. (2020) , 2021, The Cryosphere.
[5] S. Tulaczyk,et al. Inferring Ice Fabric From Birefringence Loss in Airborne Radargrams: Application to the Eastern Shear Margin of Thwaites Glacier, West Antarctica , 2021, Journal of Geophysical Research: Earth Surface.
[6] C. Schoof,et al. The role of sliding in ice stream formation , 2021, Proceedings of the Royal Society A.
[7] M. Morlighem,et al. Ice dynamics will remain a primary driver of Greenland ice sheet mass loss over the next century , 2021, Communications Earth & Environment.
[8] A. Vernal,et al. Past Warmth and Its Impacts During the Holocene Thermal Maximum in Greenland , 2020, Annual Review of Earth and Planetary Sciences.
[9] O. Eisen,et al. Complex Basal Conditions and Their Influence on Ice Flow at the Onset of the Northeast Greenland Ice Stream , 2020, Journal of Geophysical Research: Earth Surface.
[10] J. Andersen,et al. Surface velocity of the Northeast Greenland Ice Stream (NEGIS): assessment of interior velocities derived from satellite data by GPS , 2020, The Cryosphere.
[11] O. Eisen,et al. Bed topography and subglacial landforms in the onset region of the Northeast Greenland Ice Stream , 2020, Annals of Glaciology.
[12] O. Eisen,et al. Five decades of radioglaciology , 2020, Annals of Glaciology.
[13] Helene Seroussi,et al. Exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream , 2020, The Cryosphere.
[14] A. Rollett,et al. Spectral methods for full-field micromechanical modelling of polycrystalline materials , 2020 .
[15] B. Vinther,et al. A first chronology for the East Greenland Ice-core Project (EGRIP) over the Holocene and last glacial termination , 2019, Climate of the Past.
[16] N. Neckel,et al. Drainage basin delineation for outlet glaciers of Northeast Greenland based on Sentinel-1 ice velocities and TanDEM-X elevations , 2019, Remote Sensing of Environment.
[17] M. Siegert,et al. Large-scale englacial folding and deep-ice stratigraphy within the West Antarctic Ice Sheet , 2019, The Cryosphere.
[18] R. Lebensohn,et al. Shear localisation in anisotropic, non-linear viscous materials that develop a CPO: A numerical study , 2019, Journal of Structural Geology.
[19] C. Martín,et al. Basal freeze-on generates complex ice-sheet stratigraphy , 2018, Nature Communications.
[20] D. Prior,et al. Greenland Ice Sheet: Higher Nonlinearity of Ice Flow Significantly Reduces Estimated Basal Motion , 2018, Geophysical Research Letters.
[21] C. Buizert,et al. Instability of the Northeast Greenland Ice Stream over the last 45,000 years , 2018, Nature Communications.
[22] R. Lebensohn,et al. Dynamic recrystallization during deformation of polycrystalline ice: insights from numerical simulations , 2017, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[23] C. Passchier,et al. Shear zone junctions: Of zippers and freeways , 2017 .
[24] R. Lebensohn,et al. Full-field predictions of ice dynamic recrystallisation under simple shear conditions , 2016 .
[25] O. Eisen,et al. Converging flow and anisotropy cause large-scale folding in Greenland's ice sheet , 2016, Nature Communications.
[26] R. Weinberger,et al. Cycles of passive versus active diapirism recorded along an exposed salt wall , 2016 .
[27] C. Clark,et al. Ice stream activity scaled to ice sheet volume during Laurentide Ice Sheet deglaciation , 2016, Nature.
[28] M. Siegert,et al. Airborne radar evidence for tributary flow switching in Institute Ice Stream, West Antarctica: Implications for ice sheet configuration and dynamics , 2015 .
[29] D. Dahl-Jensen,et al. Response of the large-scale subglacial drainage system of Northeast Greenland to surface elevation changes , 2015 .
[30] J. Paden,et al. Radiostratigraphy and age structure of the Greenland Ice Sheet , 2015, Journal of geophysical research. Earth surface.
[31] R. Bell,et al. Traveling slippery patches produce thickness‐scale folds in ice sheets , 2014 .
[32] Sridhar Anandakrishnan,et al. Dilatant till facilitates ice-stream flow in northeast Greenland , 2014 .
[33] Helmut Schaeben,et al. Descriptive tools for the analysis of texture projects with large datasets using MTEX: strength, symmetry and components , 2014 .
[34] John Paden,et al. Deformation, warming and softening of Greenland’s ice by refreezing meltwater , 2014 .
[35] David Braaten,et al. Advanced Multifrequency Radar Instrumentation for Polar Research , 2014, IEEE Transactions on Geoscience and Remote Sensing.
[36] R. Alley,et al. Basal conditions and ice dynamics inferred from radar-derived internal stratigraphy of the northeast Greenland ice stream , 2013, Annals of Glaciology.
[37] Paul D. Bons,et al. Numerical modelling of porphyroclast and porphyroblast rotation in anisotropic rocks , 2013 .
[38] Stefano Benazzi,et al. Early dispersal of modern humans in Europe and implications for Neanderthal behaviour , 2011, Nature.
[39] Timothy D. Herbert,et al. Temperature and precipitation history of the Arctic , 2010 .
[40] T. Scambos,et al. Sequential stagnation of Kamb Ice Stream, West Antarctica , 2006 .
[41] G. Gudmundsson,et al. On the relationship between surface and basal properties on glaciers, ice sheets, and ice streams , 2005 .
[42] A. Vieli,et al. Ice Flow Direction Change in Interior West Antarctica , 2004, Science.
[43] I. Joughin,et al. High Geothermal Heat Flow, Basal Melt, and the Origin of Rapid Ice Flow in Central Greenland , 2001, Science.
[44] R. Lebensohn. N-site modeling of a 3D viscoplastic polycrystal using Fast Fourier Transform , 2001 .
[45] P. O’Higgins. The study of morphological variation in the hominid fossil record: biology, landmarks and geometry , 2000, Journal of anatomy.
[46] F. Rohlf,et al. A revolution morphometrics. , 1993, Trends in ecology & evolution.
[47] T. H. Jacka,et al. A review of ice rheology for ice sheet modelling , 1989 .
[48] John Frederick Nye,et al. The distribution of stress and velocity in glaciers and ice-sheets , 1957, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.
[49] A. Hawkins. The Results , 1952 .
[50] D. Jansen,et al. Strain localization and dynamic recrystallization in the ice – air aggregate : a numerical study , 2016 .
[51] J. Ramsay. Shear zone geometry: A review , 1980 .
[52] W. Dansgaard,et al. A Flow Model and a Time Scale for the Ice Core from Camp Century, Greenland , 1969, Journal of Glaciology.