Abstract
Models of Earth's gravity field show how the planet's density varies in its interior and on its surface, depending on topography and geologic composition. For instance, dense mountains create an area of stronger gravitational pull. Pail et al. developed a new model of Earth's gravity field using measurements from both the Gravity Recovery and Climate Experiment (GRACE) satellites and the Gravity Field and Steady‐State Ocean Circulation Explorer (GOCE) satellite.
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