Fennoscandia is the key area for glacial isostatic adjustment (GIA) research. Owing to its
long settlement and excellent infrastructure, ongoing land uplift in the north as well as …

In this review we give an overview of geophysical data and models available for the
Scandinavian mountains and adjacent areas, as they are of relevance to the debate about …

After about 6 years of GRACE (Gravity Recovery and Climate Experiment) satellite mission
operation, an unprecedented global data set on the spatio-temporal variations of the Earth's …

The gap between the Gravity Recovery and Climate Experiment (GRACE) and GRACE
Follow-on mission (GRACE-FO) is a crucial problem, leading to discontinuous global mass …

Multichannel singular spectrum analysis (MSSA) is a powerful tool to extract spatiotemporal
signals and filter errors from the noisy time-series of monthly gravity field models from the …

Summary The DEOS Mass Transport release 1 (DMT-1) model has been produced on the
basis of intersatellite K-band ranging data acquired by the GRACE satellite mission. The …

The effective elastic thickness, Te, of continental lithosphere can be estimated from the
relationship between gravity and topography in the spectral domain. Two methods have …

Based on tide gauge observations spanning almost 200 years, homogeneous time series of
the mean relative sea level were derived for nine sites at the southern coast of the Baltic …

We demonstrate a new technique for using geodetic data to update a priori predictions for
Glacial Isostatic Adjustment (GIA) in the Fennoscandia region. Global Positioning System …

Over the past two decades, the GRACE (Gravity Recovery and Climate Experiment) and
GRACE Follow-On mission (GRACE-FO) have provided monthly measurements of the …