Search Results - "Waddington, E. D."
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Past and Future Grounding-Line Retreat of the West Antarctic Ice Sheet
Published in Science (American Association for the Advancement of Science) (08-10-1999)“…The history of deglaciation of the West Antarctic Ice Sheet (WAIS) gives clues about its future. Southward grounding-line migration was dated past three…”
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Evidence for late Pleistocene thinning of Siple Dome, West Antarctica
Published in Journal of Geophysical Research - Earth Surface (01-09-2007)“…We use a two‐dimensional, full‐stress, thermomechanical flow band model to investigate late Pleistocene and Holocene histories of ice thickness and ice flow at…”
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Interpolation methods for Antarctic ice-core timescales: application to Byrd, Siple Dome and Law Dome ice cores
Published in Climate of the past (19-06-2014)“…Antarctic ice cores have often been dated by matching distinctive features of atmospheric methane to those detected in annually dated ice cores from Greenland…”
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Holocene accumulation and ice sheet dynamics in central West Antarctica
Published in Journal of Geophysical Research - Earth Surface (01-06-2008)“…We derive depth‐age relationships across the ice divide between the Ross and Amundsen Seas by tracking radar‐detected layers from the Byrd ice core and a dated…”
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Possible displacement of the climate signal in ancient ice by premelting and anomalous diffusion
Published in Nature (London) (31-05-2001)“…The best high-resolution records of climate over the past few hundred millennia are derived from ice cores retrieved from Greenland and Antarctica. The…”
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A full-stress, thermomechanical flow band model using the finite volume method
Published in Journal of Geophysical Research - Earth Surface (01-09-2007)“…A thermomechanical ice flow model is formulated using the finite volume method. Separate submodels solve the full, two‐dimensional momentum equations, the…”
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Synchronous climate changes in Antarctica and the North Atlantic
Published in Science (American Association for the Advancement of Science) (02-10-1998)“…Central Greenland ice cores provide evidence of abrupt changes in climate over the past 100,000 years. Many of these changes have also been identified in…”
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Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event
Published in Nature (London) (08-04-1993)“…Data from a Greenland ice core show that snow accumulation doubled rapidly from the Younger Dryas event to the Preboreal interval, possibly in 1-3 years. The…”
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The Accumulation Record from the GISP2 Core as an Indicator of Climate Change Throughout the Holocene
Published in Science (American Association for the Advancement of Science) (09-12-1994)“…A depth-age scale and an accumulation history for the Holocene have been established on the Greenland Ice Sheet Project 2 (GISP2) deep core, providing the most…”
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A renewed argument for crystal size control of ice sheet strain rates
Published in Journal of Geophysical Research. B (10-12-2000)“…At present, it is generally believed that crystal size has no direct influence on strain rate in the ice sheets and that the fraction of strain rate…”
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Carbonyl sulfide hydrolysis in Antarctic ice cores and an atmospheric history for the last 8000 years
Published in Journal of geophysical research. Atmospheres (16-07-2014)“…Carbonyl sulfide (COS) was measured in Antarctic ice core samples from the Byrd, Siple Dome, Taylor Dome, and West Antarctic Ice Sheet Divide sites covering…”
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Distortion of isochronous layers in ice revealed by ground-penetrating radar
Published in Nature (London) (25-03-1999)“…In addition to measuring ice-sheet thickness, ground-penetrating radar can be used to delineate reflections in ice sheets. These reflections are generally…”
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Ice Age storm trajectories inferred from radar stratigraphy at Taylor Dome, Antarctica
Published in Geophysical research letters (01-09-1998)“…The Taylor Dome ice core, East Antarctica, provides a climate record that extends through the previous interglacial. We use ice dynamics modeling and…”
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Numerical modeling of glacial erosion and headwall processes in alpine valleys
Published in Geomorphology (Amsterdam, Netherlands) (15-01-2009)“…How rock relief is developed by glacial erosion in alpine landscapes is a key question in understanding the controls on mountain range topography. Any…”
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Anomalous diffusion of multiple impurity species: Predicted implications for the ice core climate records
Published in Journal of Geophysical Research - Solid Earth (01-12-2002)“…We investigate the transport of impurities that are interpreted as climate proxies and are soluble in the premelted liquid that separates ice grains in the…”
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Electrical conductivity measurements from the GISP2 and GRIP Greenland ice cores
Published in Nature (London) (09-12-1993)“…Electrical conductivity records for the Greenland Ice Sheet Project 2 and Greenland Ice-core Project ice cores, drilled 28 km apart to enable direct comparison…”
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Grain-scale processes, folding, and stratigraphic disturbance in the GISP2 ice core
Published in Journal of Geophysical Research, Washington, DC (30-11-1997)“…Flow disturbances have been shown to alter stratigraphic order in the lower part of the ice sheet in central Greenland. Vertical thin sections of the Greenland…”
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Climate Change During the Last Deglaciation in Antarctica
Published in Science (American Association for the Advancement of Science) (14-06-1996)“…Greenland ice core records provide clear evidence of rapid changes in climate in a variety of climate indicators. In this work, rapid climate change events in…”
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A method to infer past surface mass balance and topography from internal layers in martian polar layered deposits
Published in Icarus (New York, N.Y. 1962) (01-12-2009)“…Internal layers in ice masses can be detected with ice-penetrating radar. In a flowing ice mass, each horizon represents a past surface that has been…”
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Large Arctic Temperature Change at the Wisconsin-Holocene Glacial Transition
Published in Science (American Association for the Advancement of Science) (20-10-1995)“…Analysis of borehole temperature and Greenland Ice Sheet Project II ice-core isotopic composition reveals that the warming from average glacial conditions to…”
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