Horizontal land motion observed by the 58 GNET stations used in this study, processed in the IGS14 reference frame. Credit: Journal of Geophysical Research: Solid Earth (2025). DOI: 10.1029/2024jb030847
Greenland is being twisted, compressed, and stretched. This happens due to plate tectonics and movements in the bedrock, caused by the large ice sheets on top melting and reducing pressure on the subsurface.
The pressure is easing both because large amounts of ice have melted in Greenland in recent years, and because the bedrock is still affected by the enormous ice masses that have melted since the peak of the last Ice Age about 20,000 years ago.
As a result, the entire island has shifted northwest over the past 20 years by about 2 centimeters per year.
At the same time, the movements are causing Greenland to both expand and contract horizontally. The effect is that Greenland's area is currently being "stretched out" and becoming slightly larger in some regions, while others are being "pulled together."
This is shown by new research from DTU Space, recently in the Journal of Geophysical Research: Solid Earth.
"Overall, this means Greenland is becoming slightly smaller, but that could change in the future with the accelerating melt we're seeing now," says DTU Space postdoc researcher Danjal Longfors Berg, lead author of the article.
"The ice that has melted in recent decades has pushed Greenland outward and caused uplift, so the area has actually become larger during this period. At the same time, we see movement in the opposite direction, where Greenland is rising and contracting due to prehistoric changes in the ice masses related to the last Ice Age and its end," says Berg.
Greenland has shifted northwest over the past 20 years by about 2 centimeters per year. Credit: DTU Space
It is the first time the horizontal movements have been described in such detail.
"We have created a model that shows movements over a very long timescale from about 26,000 years ago to the present. At the same time, we have used very precise measurements from the past 20 years, which we use to analyze the current movements. This means we can now measure the movements very accurately," says Berg.
The new measurements are based on 58 GNSS stations (GPS) placed around Greenland. They measure Greenland's overall position, elevation changes in the bedrock, and how the island is shrinking and stretching.
"There have not previously been such precise measurements of how Greenland is shifting. The assumption has been that Greenland is primarily being stretched due to the dynamics triggered by the ice melting in recent years. But to our surprise, we also found large areas where Greenland is being 'pulled together,' or 'shrinking,' due to the movements," says Berg.
Euler pole estimation for the North American plate. Credit: Journal of Geophysical Research: Solid Earth (2025). DOI: 10.1029/2024jb030847
The new research provides useful information about what happens when climate change hits the Arctic with accelerating speed, as is the case in these years.
"It's important to understand the movements of landmasses. They are of course interesting for geoscience. But they are also crucial for surveying and navigation, since even the fixed reference points in Greenland are slowly shifting," says Berg.
The GNSS stations are owned by the Climate Data Authority under the Ministry of Climate, Energy and Utilities. They are used for research purposes and operated in collaboration with DTU Space. The research is conducted under the DTU Space Center for Ice-Sheet and Sea-Level Predictions (CISP).
More information: D. Longfors Berg et al, Estimation and Attribution of Horizontal Land Motion Measured by the Greenland GNSS Network, Journal of Geophysical Research: Solid Earth (2025).
Journal information: Journal of Geophysical Research , Journal of Geophysical Research
Provided by Technical University of Denmark