2002b), Ice-flow characteristics over a rough bedrock: Implications for ice-core interpretation, Polar Meteorol
Recent observations in western Dronning Maud Land, Antarctica, point to a relatively high bedrock roughness in the area of the future EPICA drilling site. It is commonly accepted that such a roughness does not favor the interpretation of deep ice cores as basal ice-sheet interactions might disturb t...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.723.5027 2023-05-15T13:34:47+02:00 2002b), Ice-flow characteristics over a rough bedrock: Implications for ice-core interpretation, Polar Meteorol Frank Pattyn The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.723.5027 http://homepages.ulb.ac.be/%7Efpattyn/papers/Pattyn2002_PMG.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.723.5027 http://homepages.ulb.ac.be/%7Efpattyn/papers/Pattyn2002_PMG.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://homepages.ulb.ac.be/%7Efpattyn/papers/Pattyn2002_PMG.pdf text ftciteseerx 2021-04-04T00:19:55Z Recent observations in western Dronning Maud Land, Antarctica, point to a relatively high bedrock roughness in the area of the future EPICA drilling site. It is commonly accepted that such a roughness does not favor the interpretation of deep ice cores as basal ice-sheet interactions might disturb the bottom ice layers. The present study aims at examining the ice-flow characteristics over a strongly undulating bed and investigates its influence on age-depth profiles in the ice sheet. For this purpose a high-resolution time-dependent two-dimensional flowline model was developed (hor-izontal gridsize 1 km), taking into account all relevant stresses at such a small scale. The model is solved on a fixed finite-difference grid, and compared with a similar model, solving the velocity field accord-ing to the shallow-ice approximation. The analysis is presented for sinusoidal bedrock undulations with amplitude-to-wavelength ratio comparable to those observed by radio-echo sounding (STEINHAGE et al., 1999). Calculations are performed over a period of 300 ka. Results demonstrate that the influence of a high bed roughness on the age-depth profiles is not only confined close to the bed, but near the surface as well, which might affect the interpretation of shallow ice cores. Ice-flow characteristics over a rough bedrock 1 Text Antarc* Antarctica Dronning Maud Land EPICA ice core Ice Sheet Unknown Dronning Maud Land |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
Recent observations in western Dronning Maud Land, Antarctica, point to a relatively high bedrock roughness in the area of the future EPICA drilling site. It is commonly accepted that such a roughness does not favor the interpretation of deep ice cores as basal ice-sheet interactions might disturb the bottom ice layers. The present study aims at examining the ice-flow characteristics over a strongly undulating bed and investigates its influence on age-depth profiles in the ice sheet. For this purpose a high-resolution time-dependent two-dimensional flowline model was developed (hor-izontal gridsize 1 km), taking into account all relevant stresses at such a small scale. The model is solved on a fixed finite-difference grid, and compared with a similar model, solving the velocity field accord-ing to the shallow-ice approximation. The analysis is presented for sinusoidal bedrock undulations with amplitude-to-wavelength ratio comparable to those observed by radio-echo sounding (STEINHAGE et al., 1999). Calculations are performed over a period of 300 ka. Results demonstrate that the influence of a high bed roughness on the age-depth profiles is not only confined close to the bed, but near the surface as well, which might affect the interpretation of shallow ice cores. Ice-flow characteristics over a rough bedrock 1 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Frank Pattyn |
spellingShingle |
Frank Pattyn 2002b), Ice-flow characteristics over a rough bedrock: Implications for ice-core interpretation, Polar Meteorol |
author_facet |
Frank Pattyn |
author_sort |
Frank Pattyn |
title |
2002b), Ice-flow characteristics over a rough bedrock: Implications for ice-core interpretation, Polar Meteorol |
title_short |
2002b), Ice-flow characteristics over a rough bedrock: Implications for ice-core interpretation, Polar Meteorol |
title_full |
2002b), Ice-flow characteristics over a rough bedrock: Implications for ice-core interpretation, Polar Meteorol |
title_fullStr |
2002b), Ice-flow characteristics over a rough bedrock: Implications for ice-core interpretation, Polar Meteorol |
title_full_unstemmed |
2002b), Ice-flow characteristics over a rough bedrock: Implications for ice-core interpretation, Polar Meteorol |
title_sort |
2002b), ice-flow characteristics over a rough bedrock: implications for ice-core interpretation, polar meteorol |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.723.5027 http://homepages.ulb.ac.be/%7Efpattyn/papers/Pattyn2002_PMG.pdf |
geographic |
Dronning Maud Land |
geographic_facet |
Dronning Maud Land |
genre |
Antarc* Antarctica Dronning Maud Land EPICA ice core Ice Sheet |
genre_facet |
Antarc* Antarctica Dronning Maud Land EPICA ice core Ice Sheet |
op_source |
http://homepages.ulb.ac.be/%7Efpattyn/papers/Pattyn2002_PMG.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.723.5027 http://homepages.ulb.ac.be/%7Efpattyn/papers/Pattyn2002_PMG.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766057375240814592 |