Crustal motion and sea level changes along the Arctic coasts (CRUSLAC
The combination of tide gauges with high-precision (space-geodetic) measurements of vertical displacements of the crust and associated absolute gravity changes provide valuable con-straints for observations and models of changes in nearby ice loads. In particular, geodetic observations at tide gauge...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.532.907 2023-05-15T14:30:58+02:00 Crustal motion and sea level changes along the Arctic coasts (CRUSLAC Hans-peter Plag Surija Tatevian Oleg Zilberstein The Pennsylvania State University CiteSeerX Archives 1998 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.907 http://geodesy.unr.edu/hanspeterplag/publications/pubs/plag_weg98_crus.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.907 http://geodesy.unr.edu/hanspeterplag/publications/pubs/plag_weg98_crus.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://geodesy.unr.edu/hanspeterplag/publications/pubs/plag_weg98_crus.pdf text 1998 ftciteseerx 2016-01-08T10:41:37Z The combination of tide gauges with high-precision (space-geodetic) measurements of vertical displacements of the crust and associated absolute gravity changes provide valuable con-straints for observations and models of changes in nearby ice loads. In particular, geodetic observations at tide gauges in the Arctic are of high potential value for global change stud-ies. A preliminary analysis of the available Arctic tide gauge data indicates a spatial pattern in sea level consistent with sig-nificant changes in the ice cover on Greenland and the larger ones of the Arctic islands. However, due to lack of data on crustal motion, ambiguities remain in the separation of geo-centric crustal motion and geocentric sea levels as well as the attribution of the observed trends to past or present changes in the ice loads. It is proposed to co-located several long-operating Arctic tide gauges with continuously recording GPS, to per-form absolute gravity measurements at these selected tide gauges, and to connect all Arctic tide gauges to a geocentric datum. It is expected that these observations will allow to re-duce the uncertainty of the geocentric crustal motion and thus provide a better estimate of the geocentric sea-level trends at these tide gauges. The resulting trends will constitute valuable constraints for changes in the Arctic cryosphere. Moreover, the proposed measurements will also provide new constraints on the present-day tectonical motion of the Arctic crust. 1 Text arctic cryosphere Arctic Greenland Unknown Arctic Greenland |
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English |
description |
The combination of tide gauges with high-precision (space-geodetic) measurements of vertical displacements of the crust and associated absolute gravity changes provide valuable con-straints for observations and models of changes in nearby ice loads. In particular, geodetic observations at tide gauges in the Arctic are of high potential value for global change stud-ies. A preliminary analysis of the available Arctic tide gauge data indicates a spatial pattern in sea level consistent with sig-nificant changes in the ice cover on Greenland and the larger ones of the Arctic islands. However, due to lack of data on crustal motion, ambiguities remain in the separation of geo-centric crustal motion and geocentric sea levels as well as the attribution of the observed trends to past or present changes in the ice loads. It is proposed to co-located several long-operating Arctic tide gauges with continuously recording GPS, to per-form absolute gravity measurements at these selected tide gauges, and to connect all Arctic tide gauges to a geocentric datum. It is expected that these observations will allow to re-duce the uncertainty of the geocentric crustal motion and thus provide a better estimate of the geocentric sea-level trends at these tide gauges. The resulting trends will constitute valuable constraints for changes in the Arctic cryosphere. Moreover, the proposed measurements will also provide new constraints on the present-day tectonical motion of the Arctic crust. 1 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Hans-peter Plag Surija Tatevian Oleg Zilberstein |
spellingShingle |
Hans-peter Plag Surija Tatevian Oleg Zilberstein Crustal motion and sea level changes along the Arctic coasts (CRUSLAC |
author_facet |
Hans-peter Plag Surija Tatevian Oleg Zilberstein |
author_sort |
Hans-peter Plag |
title |
Crustal motion and sea level changes along the Arctic coasts (CRUSLAC |
title_short |
Crustal motion and sea level changes along the Arctic coasts (CRUSLAC |
title_full |
Crustal motion and sea level changes along the Arctic coasts (CRUSLAC |
title_fullStr |
Crustal motion and sea level changes along the Arctic coasts (CRUSLAC |
title_full_unstemmed |
Crustal motion and sea level changes along the Arctic coasts (CRUSLAC |
title_sort |
crustal motion and sea level changes along the arctic coasts (cruslac |
publishDate |
1998 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.907 http://geodesy.unr.edu/hanspeterplag/publications/pubs/plag_weg98_crus.pdf |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
arctic cryosphere Arctic Greenland |
genre_facet |
arctic cryosphere Arctic Greenland |
op_source |
http://geodesy.unr.edu/hanspeterplag/publications/pubs/plag_weg98_crus.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.907 http://geodesy.unr.edu/hanspeterplag/publications/pubs/plag_weg98_crus.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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1766304724835893248 |