Determination of the Earth's structure in Fennoscandia from GRACE and implications for the optimal post-processing of GRACE data

Details Determination of the Earth's structure in Fennoscandia from GRACE and implications for the optimal post-processing of GRACE data Determination of the Earth's structure in Fennoscandia from GRACE and implications for the optimal post-processing of GRACE data

Sep 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010geoji.182.1295s&link_type=abstract

Geophysical Journal International, Volume 182, Issue 3, pp. 1295-1310.

Astronomy and Astrophysics

Astronomy

2

Numerical Solutions, Satellite Geodesy, Gravity Anomalies And Earth Structure, Composition Of The Mantle, Dynamics Of Lithosphere And Mantle, Europe

Scientific paper

Analysis of data from the Gravity Recovery and Climate Experiment (GRACE) satellite mission allows us to identify regions of long-term mass changes such as the areas of Glacial Isostatic Adjustment (GIA) in North America and Fennoscandia. As there are now more than 7 yr of data available, the determined trends are robust enough for the inference of viscosity structure of the Earth's mantle. In this study, we focus on the Fennoscandian rebound area as there are abundant high-quality terrestrial data to use as ground-truth.
In the first step, GRACE data are taken to fix the optimal radial (1-D) viscosity profile and the lithospheric thickness combination, which are needed as background parameters in 3-D earth modelling. The results are in basic agreement with results based upon relative sea level and GPS data, showing a lithospheric thickness in Fennoscandia between 90 and 160 km and an upper mantle viscosity of about [2-4] × 1020 Pa s. The lower mantle viscosity is poorly resolved, however. In the second step, GRACE data are used to constrain the 3-D viscosity using spherical finite element modelling. In this case, the results also agree with past investigations, but GRACE data alone cannot discriminate between lateral heterogeneities in the mantle that are thermal in origin from those due to changes in chemical composition. More notably, we treat in detail GRACE-related questions such as implementation of an adequate Level-2 filter technique and identification of the best reduction method for hydrological mass change signals. It turns out that the Gaussian filter technique is the best for this type of investigation. Even the best global hydrology models used in GRACE investigations still fail to improve the mismatches-thus one should be careful not to blindly use them for `improving' GIA models in North America or other centres of rebound.
In conclusion, our study clearly shows that GRACE data greatly complement the study of GIA. As there are new GRACE releases in progress, and also in light of a new generation of ice history models, GRACE is likely to sharpen our insights concerning earth structure and rheology within the next few years.

Affiliated with

Also associated with

No associations

Rating

Determination of the Earth's structure in Fennoscandia from GRACE and implications for the optimal post-processing of GRACE data does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Determination of the Earth's structure in Fennoscandia from GRACE and implications for the optimal post-processing of GRACE data, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Determination of the Earth's structure in Fennoscandia from GRACE and implications for the optimal post-processing of GRACE data will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1495113