Year: 2024
Type: software-paper
Abstract: The acceleration due to gravity is not uniform across Earth's surface because of local variations in topography and in the density distribution within the Earth.Measurements of local gravity anomalies -the difference between theoretically predicted gravity and observed gravity -can therefore be used to infer density variations in Earth's interior which influence tectonic and geodynamic processes (e.g.
DOI: 10.21105/joss.07358
Authors: Hannah F. Mark, Jasmine Zhu, Masako Tominaga, Daniel Aliod, Maurice Tivey
Institution: Woods Hole Oceanographic Institution
Language: English
Subfield: Oceanography
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: diamond
OpenAlex ID: W4404627082