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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Main Authors: Hans-peter Plag, Surija Tatevian, Oleg Zilberstein
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1998
Subjects:
Online Access: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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spelling 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
institution Open Polar
collection Unknown
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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
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