Planetary g(t) for which resistive atmospheric falling is rising
| dc.creator | Rosu, H. C. | |
| dc.creator | de la Cruz, F. Aceves | |
| dc.date | 2001-08-17 | |
| dc.date | 2001-08-23 | |
| dc.date.accessioned | 2026-07-07T03:26:16Z | |
| dc.date.available | 2026-07-07T03:26:16Z | |
| dc.description | A Darboux-transformed surface gravitational acceleration of the constant gravitational acceleration for a body endowed with an atmospheric layer is shown to turn the atmospheric free fall with quadratic resistance in the opposite motion, i.e., a free rising. Although the atmosphere of such a body may look completely normal, it is the time dependence of its gravitational field that produces this type of motion. The result is a consequence of general, one-parameter-dependent Darboux transformations in mathematical physics | |
| dc.description | 9 pages, 6 figures, change of format and correction of Eqs. 21 and 22, not affecting the plots | |
| dc.identifier | https://arxiv.org/abs/gr-qc/0108044 | |
| dc.identifier | http://arxiv.org/abs/gr-qc/0108044 | |
| dc.identifier.uri | http://salesiana.dossiersoluciones.com/handle/123456789/33977 | |
| dc.subject | General Relativity and Quantum Cosmology | |
| dc.title | Planetary g(t) for which resistive atmospheric falling is rising | |
| dc.type | text |