In a context of global change and increasing anthropic pressure on the environment,
monitoring the Earth system and its evolution has become one of the key missions of …

Paleogeographic maps play a central integrating role across all the disciplines of the Earth
System Sciences. They increasingly serve as boundary conditions for climate, earth, and life …

The observed crustal uplift rates in Greenland are caused by the combined response of the
solid Earth to both ongoing and past surface mass changes. Existing elastic Earth models …

Climate change threatens many well‐preserved archaeological sites in the Arctic. The paper
presents the first Arctic multi‐threat assessment focusing on the Nuuk region of Greenland …

Mass transport estimates based on filtered Gravity Recovery and Climate Experiment
(GRACE) monthly spherical harmonic gravity field solutions generally suffer from resolution …

Time-variable gravity field models obtained from satellite gravimetric techniques allow for
the assessment of ice sheet mass changes in remote polar regions, such as Greenland and …

Greenland's outlet glaciers have been a leading source of mass loss and accompanying sea‐
level rise from the Greenland Ice Sheet (GrIS) over the last 25 years. The dynamic …

During the past 120 Ma, the Greenland craton drifted over the Iceland hot spot; however,
uncertainties in geodynamic modeling and a lack of geophysical evidence prevent an …

Crustal motion generated by rapid ice‐mass loss from Earth's glaciers and ice sheets has
previously been considered in Global Navigational Satellite System (GNSS) analyses and …

Determining reliable probability distributions for ice sheet mass change over the coming
century is critical to refining uncertainties in sea-level rise projections. Bayesian calibration …