{"push_id":815795754,"size":1,"distinct_size":1,"ref":"refs/heads/master","head":"9782832734046acdd9158377b8f3fc97dc118cad","before":"7fd8cabd2e3501db709fe704143ed9ce627de9e0","commits":[{"sha":"9782832734046acdd9158377b8f3fc97dc118cad","author":{"email":"3905346d7a284e66cb11b2a5d321f9ea00e4b6c5@gmail.com","name":"Phlos"},"message":"added gravity potential\n\nInstead of the full gravity vector, gravity data are now also generated that are based on the gravity potential calculated at the location of the gravity receivers.\n\nto this end, g_obs now has not only components .x, .z and .mag (which describe the gravity vector and its magnitude), but also .pot (which is the gravity potential, calculated as int_V - G * rho(r) / |r| dx dz . Depending on whether which_grav = 'g_vector' or 'g_potential', one or the other will be used (for instance in calculating misfit_grav).\n\nFiles changed to this end: eval_objective_and_gradient; eval_gradient; calc_misfits; compute_kernels_gravity; make_gravity_sources.","distinct":true,"url":"https://api.github.com/repos/Phlos/fd2d-adjoint/commits/9782832734046acdd9158377b8f3fc97dc118cad"}]}