The Postglacial Rebound Signal of Fennoscandia Observed by Absolute Gravimetry, GPS, and Tide Gauges
Author
Source
International Journal of Geophysics
Issue
Vol. 2011, Issue 2011 (31 Dec. 2011), pp.1-3, 3 p.
Publisher
Hindawi Publishing Corporation
Publication Date
2010-11-29
Country of Publication
Egypt
No. of Pages
3
Main Subjects
Abstract EN
We have compiled time derivatives of gravity and vertical motion for a dozen sites in Fennoscandia.
Time series of absolute gravimetry and permanent GPS cover a time span of about a decade.
Tide gauges have operated for many decades near seven of the sites.
Linear relations are found to range from −0.17 to −0.22 for the slope between gravity and vertical uplift rates.
An eustatic sea level rate of 1.2 mm/year is derived from these data.
This compares well with results for North America and with theoretical predictions for viscoelastic Earth models.
American Psychological Association (APA)
Pettersen, Bjørn Ragnvald. 2010. The Postglacial Rebound Signal of Fennoscandia Observed by Absolute Gravimetry, GPS, and Tide Gauges. International Journal of Geophysics،Vol. 2011, no. 2011, pp.1-3.
https://search.emarefa.net/detail/BIM-511333
Modern Language Association (MLA)
Pettersen, Bjørn Ragnvald. The Postglacial Rebound Signal of Fennoscandia Observed by Absolute Gravimetry, GPS, and Tide Gauges. International Journal of Geophysics No. 2011 (2011), pp.1-3.
https://search.emarefa.net/detail/BIM-511333
American Medical Association (AMA)
Pettersen, Bjørn Ragnvald. The Postglacial Rebound Signal of Fennoscandia Observed by Absolute Gravimetry, GPS, and Tide Gauges. International Journal of Geophysics. 2010. Vol. 2011, no. 2011, pp.1-3.
https://search.emarefa.net/detail/BIM-511333
Data Type
Journal Articles
Language
English
Notes
Includes bibliographical references
Record ID
BIM-511333