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 ...
Abstract: As parallel to recent advances in space technologies, satellite systems has become a very efficient technique for precise positioning in Geodesy Science. Global Positioning System (GPS) ...
A peer-reviewed study published in Scientific Reports has reconstructed the evolution of the Antarctic Geoid Low, the strongest negative gravity anomaly on Earth, over approximately 70 million years, ...
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 ...