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Abstract. Radio echo surveys to determine the thickness of ice sheets often record reflections from inside the ice. To increase our understanding of these internal reflections we have used synthetic seismogram techniques from early seismic modeling to construct two models. Both models were one-dimen...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.366.8142 2023-05-15T16:28:11+02:00 4 W. D. Miners E. W. Wolff J. C. Moore R. Jacobel L. Hempel The Pennsylvania State University CiteSeerX Archives http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.366.8142 http://www.stolaf.edu/other/cegsic/publications/Miners et al.PDF en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.366.8142 http://www.stolaf.edu/other/cegsic/publications/Miners et al.PDF Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.stolaf.edu/other/cegsic/publications/Miners et al.PDF text ftciteseerx 2016-01-08T01:05:11Z Abstract. Radio echo surveys to determine the thickness of ice sheets often record reflections from inside the ice. To increase our understanding of these internal reflections we have used synthetic seismogram techniques from early seismic modeling to construct two models. Both models were one-dimensional; the first considered only primary reflections, while the second included both primary and multiple reflections. The inputs to both models were a radio pulse and data from the Greenland Ice core Project (GRIP) core of length 3028 m. The ice core data was a profile of the high frequency conductivity, calculated from dielectric profile (DEP) 2 1 2 Text Greenland Greenland ice core Greenland Ice core Project GRIP ice core Unknown Greenland |
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ftciteseerx |
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description |
Abstract. Radio echo surveys to determine the thickness of ice sheets often record reflections from inside the ice. To increase our understanding of these internal reflections we have used synthetic seismogram techniques from early seismic modeling to construct two models. Both models were one-dimensional; the first considered only primary reflections, while the second included both primary and multiple reflections. The inputs to both models were a radio pulse and data from the Greenland Ice core Project (GRIP) core of length 3028 m. The ice core data was a profile of the high frequency conductivity, calculated from dielectric profile (DEP) 2 1 2 |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
author |
W. D. Miners E. W. Wolff J. C. Moore R. Jacobel L. Hempel |
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W. D. Miners E. W. Wolff J. C. Moore R. Jacobel L. Hempel 4 |
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W. D. Miners E. W. Wolff J. C. Moore R. Jacobel L. Hempel |
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W. D. Miners |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.366.8142 http://www.stolaf.edu/other/cegsic/publications/Miners et al.PDF |
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Greenland |
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Greenland |
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Greenland Greenland ice core Greenland Ice core Project GRIP ice core |
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Greenland Greenland ice core Greenland Ice core Project GRIP ice core |
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http://www.stolaf.edu/other/cegsic/publications/Miners et al.PDF |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.366.8142 http://www.stolaf.edu/other/cegsic/publications/Miners et al.PDF |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766017807504375808 |