Scientists are using the Antarctic Geoid Low, a gravity hole, to track changes in Earth's deep interior over millions of years.

Abstract: High-resolution sea surface heights (SSHs) can be obtained from the wide-swath data of the surface water and ocean topography (SWOT) project. The distance between two points used to ...

Scientists have finally explained the Indian Ocean Geoid Low, a significant gravity anomaly, linking its formation to deep Earth processes and ancient tectonic plate movements.

Scientists have finally explained the Indian Ocean Geoid Low, a massive gravity anomaly south of India. New research reveals this 'gravity hole' formed over millions of years due to hot, less dense ...

The geoid (the surface of equal gravitational potential of a hypothetical ocean at rest) serves as the classical reference ...

A mysterious gravity dip beneath Antarctica is growing stronger, shaped by deep Earth forces over millions of years.

One of the strongest of these depressions – where the gravity field is weaker – lies under Antarctica. Now, new models of how the so-called Antarctic Geoid Low evolved over time have shown that it's ...

Antarctica sits above the strongest negative gravity anomaly on Earth, a region where the planet’s gravitational pull dips so ...

This strange 'gravity hole' beneath Antarctica could help explain how its ice and oceans changed over millions of years.

Antarctica is home to many mysteries, but one of the strangest is an enormous 'gravity hole' deep beneath the ice. Now, ...

A new study has reconstructed the evolution of the planet’s strongest nonhydrostatic geoid depression —the Antarctic Geoid ...