Journal cover Journal topic
Solid Earth An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 2.380 IF 2.380
  • IF 5-year value: 3.147 IF 5-year
    3.147
  • CiteScore value: 3.06 CiteScore
    3.06
  • SNIP value: 1.335 SNIP 1.335
  • IPP value: 2.81 IPP 2.81
  • SJR value: 0.779 SJR 0.779
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 32 Scimago H
    index 32
  • h5-index value: 31 h5-index 31
Volume 9, issue 3
Solid Earth, 9, 777–795, 2018
https://doi.org/10.5194/se-9-777-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Solid Earth, 9, 777–795, 2018
https://doi.org/10.5194/se-9-777-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 15 Jun 2018

Research article | 15 Jun 2018

The glacial isostatic adjustment signal at present day in northern Europe and the British Isles estimated from geodetic observations and geophysical models

Karen M. Simon et al.
Viewed  
Total article views: 1,742 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,342 379 21 1,742 28 35
  • HTML: 1,342
  • PDF: 379
  • XML: 21
  • Total: 1,742
  • BibTeX: 28
  • EndNote: 35
Views and downloads (calculated since 07 Feb 2018)
Cumulative views and downloads (calculated since 07 Feb 2018)
Viewed (geographical distribution)  
Total article views: 1,614 (including HTML, PDF, and XML) Thereof 1,609 with geography defined and 5 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Cited  
Saved (final revised paper)  
No saved metrics found.
Saved (discussion paper)  
No saved metrics found.
Discussed (final revised paper)  
Discussed (discussion paper)  
No discussed metrics found.
Latest update: 22 Aug 2019
Publications Copernicus
Download
Short summary
This study constrains the post-glacial rebound signal in Scandinavia and northern Europe via the combined inversion of prior forward model information with GPS-measured vertical land motion data and GRACE gravity data. The best-fit model for vertical motion rates has a χ2 value of ~ 1 and a maximum uncertainty of 0.3–0.4 mm yr−1. An advantage of inverse models relative to forward models is their ability to estimate formal uncertainties associated with the post-glacial rebound process.
This study constrains the post-glacial rebound signal in Scandinavia and northern Europe via the...
Citation