[4] Donald Lynden-Bell, a British theoretical astrophysicist, constructed the equation[6] for calculating the conditions and effects of self gravitation.
The equation's main purpose is to give exact descriptions of models for rotating flattened globular clusters.
Self-gravity affects bodies passing each other in space, within the sphere defined by their Roche limit.
[4] Additionally, in most astronomical circumstances the transit through a Roche limit is temporary, so the force of self-gravitation can restore the body's composition after the fact.
[12] Self-gravity is influential in understanding the sea level and ice caps for oceanographers and geologists, which is particularly important for anticipating the effects of climate change.