We derive, supported on a generalization of Bernoulli’s equation, a law of rotation for any axial-symmetric, self-gravitating fluid mass. For a homogeneous mass, the law depends solely on the derivative of the potential with respect to the distance to the rotation axis, implying generally differential rotation, the Maclaurin spheroids representing the only case of solid-body rotation. We turn then to a heterogeneous mass consisting of any number l of concentric layers, each of constant density, finding that the angular velocity profile of a given layer depends on that of the layer immediately above it. Finally, we let l tend to infinity to convert our model into continuous mass distribution, the result being a certain rotation profile for the surface, and law of differential rotation change at its interior. To support the fundamentals of our approach, we write the potential integrals for the three mass distributions. The aim of a continuous distribution is that it may facilitate a comparison---to be carried out in a future paper---between our results and those of other researchers who employ structure equations. We point out that the distribution of angular velocity is a consequence of the equilibrium, rather than being imposed ad initio. The law was used in a past paper to construct a Jupiter multi-layer model adopting the spheroidal (a distorted spheroid) shape for each of the layers, taking as reference the gravitational data surveyed by the Juno mission. The procedure used here is not restricted to axial-symmetric cases.
Published in | American Journal of Astronomy and Astrophysics (Volume 8, Issue 2) |
DOI | 10.11648/j.ajaa.20200802.13 |
Page(s) | 30-34 |
Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
Copyright |
Copyright © The Author(s), 2020. Published by Science Publishing Group |
Gravitation, Hydrodynamics, Planets and Satellites, Stars, Rotation
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APA Style
Joel Uriel Cisneros-Parra, Francisco Javier Martínez-Herrera, Daniel Montalvo-Castro. (2020). A Differential Rotation Law for Stars and Fluid Planets. American Journal of Astronomy and Astrophysics, 8(2), 30-34. https://doi.org/10.11648/j.ajaa.20200802.13
ACS Style
Joel Uriel Cisneros-Parra; Francisco Javier Martínez-Herrera; Daniel Montalvo-Castro. A Differential Rotation Law for Stars and Fluid Planets. Am. J. Astron. Astrophys. 2020, 8(2), 30-34. doi: 10.11648/j.ajaa.20200802.13
AMA Style
Joel Uriel Cisneros-Parra, Francisco Javier Martínez-Herrera, Daniel Montalvo-Castro. A Differential Rotation Law for Stars and Fluid Planets. Am J Astron Astrophys. 2020;8(2):30-34. doi: 10.11648/j.ajaa.20200802.13
@article{10.11648/j.ajaa.20200802.13, author = {Joel Uriel Cisneros-Parra and Francisco Javier Martínez-Herrera and Daniel Montalvo-Castro}, title = {A Differential Rotation Law for Stars and Fluid Planets}, journal = {American Journal of Astronomy and Astrophysics}, volume = {8}, number = {2}, pages = {30-34}, doi = {10.11648/j.ajaa.20200802.13}, url = {https://doi.org/10.11648/j.ajaa.20200802.13}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajaa.20200802.13}, abstract = {We derive, supported on a generalization of Bernoulli’s equation, a law of rotation for any axial-symmetric, self-gravitating fluid mass. For a homogeneous mass, the law depends solely on the derivative of the potential with respect to the distance to the rotation axis, implying generally differential rotation, the Maclaurin spheroids representing the only case of solid-body rotation. We turn then to a heterogeneous mass consisting of any number l of concentric layers, each of constant density, finding that the angular velocity profile of a given layer depends on that of the layer immediately above it. Finally, we let l tend to infinity to convert our model into continuous mass distribution, the result being a certain rotation profile for the surface, and law of differential rotation change at its interior. To support the fundamentals of our approach, we write the potential integrals for the three mass distributions. The aim of a continuous distribution is that it may facilitate a comparison---to be carried out in a future paper---between our results and those of other researchers who employ structure equations. We point out that the distribution of angular velocity is a consequence of the equilibrium, rather than being imposed ad initio. The law was used in a past paper to construct a Jupiter multi-layer model adopting the spheroidal (a distorted spheroid) shape for each of the layers, taking as reference the gravitational data surveyed by the Juno mission. The procedure used here is not restricted to axial-symmetric cases.}, year = {2020} }
TY - JOUR T1 - A Differential Rotation Law for Stars and Fluid Planets AU - Joel Uriel Cisneros-Parra AU - Francisco Javier Martínez-Herrera AU - Daniel Montalvo-Castro Y1 - 2020/05/15 PY - 2020 N1 - https://doi.org/10.11648/j.ajaa.20200802.13 DO - 10.11648/j.ajaa.20200802.13 T2 - American Journal of Astronomy and Astrophysics JF - American Journal of Astronomy and Astrophysics JO - American Journal of Astronomy and Astrophysics SP - 30 EP - 34 PB - Science Publishing Group SN - 2376-4686 UR - https://doi.org/10.11648/j.ajaa.20200802.13 AB - We derive, supported on a generalization of Bernoulli’s equation, a law of rotation for any axial-symmetric, self-gravitating fluid mass. For a homogeneous mass, the law depends solely on the derivative of the potential with respect to the distance to the rotation axis, implying generally differential rotation, the Maclaurin spheroids representing the only case of solid-body rotation. We turn then to a heterogeneous mass consisting of any number l of concentric layers, each of constant density, finding that the angular velocity profile of a given layer depends on that of the layer immediately above it. Finally, we let l tend to infinity to convert our model into continuous mass distribution, the result being a certain rotation profile for the surface, and law of differential rotation change at its interior. To support the fundamentals of our approach, we write the potential integrals for the three mass distributions. The aim of a continuous distribution is that it may facilitate a comparison---to be carried out in a future paper---between our results and those of other researchers who employ structure equations. We point out that the distribution of angular velocity is a consequence of the equilibrium, rather than being imposed ad initio. The law was used in a past paper to construct a Jupiter multi-layer model adopting the spheroidal (a distorted spheroid) shape for each of the layers, taking as reference the gravitational data surveyed by the Juno mission. The procedure used here is not restricted to axial-symmetric cases. VL - 8 IS - 2 ER -