The Postglacial Rebound Signal of Fennoscandia Observed by Absolute Gravimetry, GPS, and Tide Gauges
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 −...
Saved in:
| Main Author: | Bjørn Ragnvald Pettersen |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Wiley
2011-01-01
|
| Series: | International Journal of Geophysics |
| Online Access: | http://dx.doi.org/10.1155/2011/957329 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
A Probabilistic Approach to Characterizing Drought Using Satellite Gravimetry
by: Peyman Saemian, et al.
Published: (2024-08-01) -
Estimation of Relative Sea Level Change in Locations Without Tide Gauges Using Artificial Neural Networks
by: Heeryun Kim, et al.
Published: (2025-06-01) -
Autumn migration patterns of buntings (Emberiza spp.) in eastern Fennoscandia
by: Юлия Михайловна Банникова
Published: (2025-08-01) -
TRACES OF SEISMIC ACTIVITY IN THE LAKE BOTTOM SEDIMENTS OF EASTERN FENNOSCANDIA
by: S. B. Nikolaeva
Published: (2022-12-01) -
Postglacial relative sea level change at Fildes Peninsula, King George Island (West Antarctic)
by: K. V. Polishchuk, et al.
Published: (2016-02-01)