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7 Titles Match Your Query
Showing 1 through 7 of 7
1. Sonic Log Data for the NEEM Corehole [pettit_1208635]
This dataset contains a record of speeds for vertically-propagating compression waves measured throughout the depth of ice that surrounds the NEEM corehole. Multiple logs provide redundant measurements ...


2. WAIS Divide Sonic Log Data [waddington_0944199]
This dataset contains a record of speeds for vertically-propagating compression-waves measured throughout the depth of ice that surrounds the WAIS-D corehole. Multiple logs provide redundant measurements ...


3. Millennially averaged accumulation rates for the Lake Vostok region inferred from deep internal layers [Vostok_accum]
The depths of radar-detected internal layers can be used to infer the spatial variability of accumulation rates. Here we infer accumulation rates from three radar layers (26, 35 and 41ka old) in the ...


4. Modeled radar attenuation-rate profile at the Vostok 5G ice-core site [Vostok_atten]
The modeled radar attenuation-rate profile presented here shows the predicted contributions from pure ice and impurities to radar attenuation at the Vostok 5G ice-core site, as well as the total attenuation ...


5. Glacial history of Conway Ice Ridge, West Antarctica [conway_OPP008714]
The primary goal of the work was to investigate the glacial history of Conway Ridge, the ice ridge between Mercer Ice Stream and Van der Veen Ice Stream. Primary investigative tools were: high and ...


6. Inland migration of fast-flowing outlet glaciers and ice streams: Model investigations of the transition from tributary to ice-stream flow [waddington_OPP0125610]
We have developed a two-dimensional full-stress model to (1) investigate the controlling processes in onset regions and (2) examine how those processes might affect the evolution of the onset region ...


7. Investigation of the glacial history of the Siple Coast using radar-detected internal layers and the ice core from Siple Dome [conway_OPP0229490]
We are using ice-penetrating radar data collected over the course of several field seasons in West Antarctica to analyze and detect englacial radar layers. These radar layers are due to fluctuations ...


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