How Ancient Volcanic Paths Beneath Greenland Are Reshaping Our Future Sea Level Forecasts

Science Bulletins: Mapping the Heat Beneath · 9:41 · Video: American Museum of Natural History · Watch at the source

In short: Deep beneath Greenland’s massive ice sheet, uneven heat is rising from the Earth’s interior. By mapping this thermal landscape, scientists have discovered that the island’s ancient journey over a volcanic hotspot is still influencing how ice moves and melts today, providing a critical new variable for climate change predictions.

Geophysicists have long used seismic waves to peer into the Earth's interior, revealing hidden dynamics like melting mantle and deep-diving rock. Recently, a research team led by the University of Ottawa, in collaboration with the University of Twente and the Geological Survey of Denmark and Greenland, applied this approach to Greenland. By combining satellite observations with ground-based data, they generated the most detailed 3D models of temperatures beneath the island and northeastern Canada to date.

The team ran hundreds of thousands of computer simulations, utilizing high-performance systems from the Digital Research Alliance of Canada. These models show that heat is not distributed evenly beneath the ice. Instead, the thermal structure is marked by significant lateral variations, which the study’s lead author, Parviz Ajourlou, attributes to Greenland’s historical passage over the Iceland hotspot. This geological journey left a lasting imprint on the geophysical properties of the underlying bedrock.

Understanding this subterranean heat is vital for climate science. The temperature at the base of the ice sheet dictates how the ice slides and how the ground beneath it shifts. By integrating these thermal models with seismic velocities, gravity anomalies, and heat flow data, researchers can better interpret satellite measurements of land motion. This refinement is essential for quantifying how the ice sheet responds to modern warming.

Ultimately, this research bridges the gap between solid Earth geophysics and climate systems. As principal investigator Glenn Milne notes, accounting for these ice-earth interactions allows scientists to improve simulations of ice loss. By refining these models, researchers can produce more accurate forecasts of Greenland's contribution to global sea level rise, offering a clearer picture of what the future holds for coastal regions worldwide.

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