Equilibrium Tides on Planets and Stars
Autor(a) principal: | |
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Data de Publicação: | 2022 |
Tipo de documento: | Tese |
Idioma: | eng |
Título da fonte: | Biblioteca Digital de Teses e Dissertações da USP |
Texto Completo: | https://doi.org/10.11606/T.14.2022.tde-20062022-170909 |
Resumo: | Most applications currently made using equilibrium tidal theories are based on the use of ad-hoc tidal lags. In the case of applications made with Darwin\'s classical theory, for example, the prediction for the final stage of rotational evolution is synchronism for the case of circular orbits and supersynchronism for eccentric orbits (where the excess of rotation in relation to the synchronism is given by 6ne2, where n is the mean orbital motion and is the orbital eccentricity). Recently, a formulation for equilibrium tides that considers a linearized solution of the Navier-Stokes equation was made at the IAG (see Ferraz-Mello 2013, 2015). The theory allows the description of equilibrium tides in both rigid bodies (such as super-Earths) and gaseous bodies (such as mini-Neptunes and hot Jupiters) by adjusting just one parameter, which is the uniform viscosity coefficient. The first version of the tidal creep theory (ie the version proposed in Ferraz-Mello 2013, 2015) was based on a series expansion of the so-called creep equation. In this structure, the rate of rotation of the tidal deformed body was considered constant when solving the creep equation. Then, the rotation rate was evolved considering the torque expression related to tidal interactions. This method is not consistent when it comes to the evolution of the rotation rate of the tidal deformed body. One of the consequences of considering the rotation rate constant for the body when solving the creep equation is that the rotation rate librations in the synchronous rotation regime are very small for rigid bodies. This result is inconsistent with the libration amplitude of the rotation rate and the tidal lag angle of the Solar System\'s planetary satellites. A new formulation of the tidal creep theory was proposed in Folonier et al. (2018). The new version of the theory leads to a consistent treatment of the rotational dynamics of the tidally deformed body, where forced librations around the synchronous solution (which are characteristic in the case of rigid bodies such as super-Earths and planetary satellites) are reproduced. Furthermore, the new version of the tidal creep theory allows a study of the equilibrium figure of the tidal deformed body in a much simpler way than the previous version of the theory. In this thesis, we present applications of the tidal creep theory to several cases, where both gas giant planets and Earth-like rigid planets are considered. We also discuss in detail the differences between the first version of the creep tide theory (see Ferraz-Mello 2013, 2015) and the new version (see Folonier et al. 2018). |
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info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesis Equilibrium Tides on Planets and Stars Marés de Equilíbrio em Planetas e Estrelas 2022-05-06Sylvio Ferraz de MelloAmaury Augusto de AlmeidaEmeline BolmontHugo Alberto FolonierNelson Vani LeisterTadashi YokoyamaGabriel de Oliveira GomesUniversidade de São PauloAstronomiaUSPBR Creep Creep Equilíbrio Equilibrium Evolucão Evolution Marés Orbit Órbita Rotação Spin Tides Most applications currently made using equilibrium tidal theories are based on the use of ad-hoc tidal lags. In the case of applications made with Darwin\'s classical theory, for example, the prediction for the final stage of rotational evolution is synchronism for the case of circular orbits and supersynchronism for eccentric orbits (where the excess of rotation in relation to the synchronism is given by 6ne2, where n is the mean orbital motion and is the orbital eccentricity). Recently, a formulation for equilibrium tides that considers a linearized solution of the Navier-Stokes equation was made at the IAG (see Ferraz-Mello 2013, 2015). The theory allows the description of equilibrium tides in both rigid bodies (such as super-Earths) and gaseous bodies (such as mini-Neptunes and hot Jupiters) by adjusting just one parameter, which is the uniform viscosity coefficient. The first version of the tidal creep theory (ie the version proposed in Ferraz-Mello 2013, 2015) was based on a series expansion of the so-called creep equation. In this structure, the rate of rotation of the tidal deformed body was considered constant when solving the creep equation. Then, the rotation rate was evolved considering the torque expression related to tidal interactions. This method is not consistent when it comes to the evolution of the rotation rate of the tidal deformed body. One of the consequences of considering the rotation rate constant for the body when solving the creep equation is that the rotation rate librations in the synchronous rotation regime are very small for rigid bodies. This result is inconsistent with the libration amplitude of the rotation rate and the tidal lag angle of the Solar System\'s planetary satellites. A new formulation of the tidal creep theory was proposed in Folonier et al. (2018). The new version of the theory leads to a consistent treatment of the rotational dynamics of the tidally deformed body, where forced librations around the synchronous solution (which are characteristic in the case of rigid bodies such as super-Earths and planetary satellites) are reproduced. Furthermore, the new version of the tidal creep theory allows a study of the equilibrium figure of the tidal deformed body in a much simpler way than the previous version of the theory. In this thesis, we present applications of the tidal creep theory to several cases, where both gas giant planets and Earth-like rigid planets are considered. We also discuss in detail the differences between the first version of the creep tide theory (see Ferraz-Mello 2013, 2015) and the new version (see Folonier et al. 2018). A maioria das aplicações atualmente feitas usando teorias de marés de equilíbrio são baseadas no uso de defasagens de maré ad-hoc. Nos casos de aplicações feitas com a teoria clássica de Darwin, por exemplo, a previsão para o estágio final da evolução rotacional é o sincronismo para o caso de órbitas circulares e o supersincronismo para órbitas excêntricas (onde o excesso de rotação em relação ao sincronismo é dado por 6ne2, onde n é o movimento orbital médio e e a excentricidade orbital). Recentemente, uma formulação para marés de equilíbrio que considera uma solução linearizada da equação de Navier-Stokes foi feita no IAG (ver Ferraz-Mello 2013, 2015). A teoria permite a descrição de marés de equilíbrio tanto em corpos rígidos (como super-Terras) quanto em corpos gasosos (como mini-Netunos e Júpiteres quentes) ajustando apenas um parâmetro, que é o coeficiente de viscosidade uniforme. A primeira versão da teoria da maré de fluência (ou seja, a versão proposta em Ferraz-Mello 2013, 2015) foi baseada em uma expansão em série da chamada equação de fluência. Nessa estrutura, a taxa de rotação do corpo deformado por maré foi considerada constante ao resolver a equação de fluência. Em seguida, a taxa de rotação foi evoluída considerando a expressão de torque relacionada às interações de maré. Este método não é consistente quando se trata da evolução da taxa de rotação do corpo deformado por maré. Uma das consequências de considerar a taxa de rotação constante para o corpo ao resolver a equação da fluência é que as librações da taxa de rotação no regime de rotação síncrona são muito pequenas para corpos rígidos. Este resultado é inconsistente com a amplitude de libração da taxa de rotação e o ângulo de defasagem das marés dos satélites planetários do Sistema Solar. Uma nova formulação da teoria da maré de fluência foi proposta em Folonier et al. (2018). A nova versão da teoria leva a um tratamento consistente da dinâmica de rotação do corpo deformado por maré, onde librações forçadas em torno da solução síncrona (que são características no caso de corpos rígidos, como super-Terras e satélites planetários) são reproduzidas. Além disso, a nova versão da teoria da maré de fluência permite um estudo da figura de equilíbrio do corpo deformado por maré de uma maneira muito mais simples do que a versão anterior da teoria. Nesta tese, apresentamos aplicações da teoria das marés de fluência a vários casos, onde são considerados tanto planetas gigantes gasosos quanto planetas rígidos semelhantes à Terra. Também discutimos em detalhes as diferenças entre a primeira versão da teoria da maré de fluência (ver Ferraz-Mello 2013, 2015) e a nova versão (ver Folonier et al. 2018). https://doi.org/10.11606/T.14.2022.tde-20062022-170909info:eu-repo/semantics/openAccessengreponame:Biblioteca Digital de Teses e Dissertações da USPinstname:Universidade de São Paulo (USP)instacron:USP2023-12-21T19:31:44Zoai:teses.usp.br:tde-20062022-170909Biblioteca Digital de Teses e Dissertaçõeshttp://www.teses.usp.br/PUBhttp://www.teses.usp.br/cgi-bin/mtd2br.plvirginia@if.usp.br|| atendimento@aguia.usp.br||virginia@if.usp.bropendoar:27212023-12-22T12:58:21.669270Biblioteca Digital de Teses e Dissertações da USP - Universidade de São Paulo (USP)false |
dc.title.en.fl_str_mv |
Equilibrium Tides on Planets and Stars |
dc.title.alternative.pt.fl_str_mv |
Marés de Equilíbrio em Planetas e Estrelas |
title |
Equilibrium Tides on Planets and Stars |
spellingShingle |
Equilibrium Tides on Planets and Stars Gabriel de Oliveira Gomes |
title_short |
Equilibrium Tides on Planets and Stars |
title_full |
Equilibrium Tides on Planets and Stars |
title_fullStr |
Equilibrium Tides on Planets and Stars |
title_full_unstemmed |
Equilibrium Tides on Planets and Stars |
title_sort |
Equilibrium Tides on Planets and Stars |
author |
Gabriel de Oliveira Gomes |
author_facet |
Gabriel de Oliveira Gomes |
author_role |
author |
dc.contributor.advisor1.fl_str_mv |
Sylvio Ferraz de Mello |
dc.contributor.referee1.fl_str_mv |
Amaury Augusto de Almeida |
dc.contributor.referee2.fl_str_mv |
Emeline Bolmont |
dc.contributor.referee3.fl_str_mv |
Hugo Alberto Folonier |
dc.contributor.referee4.fl_str_mv |
Nelson Vani Leister |
dc.contributor.referee5.fl_str_mv |
Tadashi Yokoyama |
dc.contributor.author.fl_str_mv |
Gabriel de Oliveira Gomes |
contributor_str_mv |
Sylvio Ferraz de Mello Amaury Augusto de Almeida Emeline Bolmont Hugo Alberto Folonier Nelson Vani Leister Tadashi Yokoyama |
description |
Most applications currently made using equilibrium tidal theories are based on the use of ad-hoc tidal lags. In the case of applications made with Darwin\'s classical theory, for example, the prediction for the final stage of rotational evolution is synchronism for the case of circular orbits and supersynchronism for eccentric orbits (where the excess of rotation in relation to the synchronism is given by 6ne2, where n is the mean orbital motion and is the orbital eccentricity). Recently, a formulation for equilibrium tides that considers a linearized solution of the Navier-Stokes equation was made at the IAG (see Ferraz-Mello 2013, 2015). The theory allows the description of equilibrium tides in both rigid bodies (such as super-Earths) and gaseous bodies (such as mini-Neptunes and hot Jupiters) by adjusting just one parameter, which is the uniform viscosity coefficient. The first version of the tidal creep theory (ie the version proposed in Ferraz-Mello 2013, 2015) was based on a series expansion of the so-called creep equation. In this structure, the rate of rotation of the tidal deformed body was considered constant when solving the creep equation. Then, the rotation rate was evolved considering the torque expression related to tidal interactions. This method is not consistent when it comes to the evolution of the rotation rate of the tidal deformed body. One of the consequences of considering the rotation rate constant for the body when solving the creep equation is that the rotation rate librations in the synchronous rotation regime are very small for rigid bodies. This result is inconsistent with the libration amplitude of the rotation rate and the tidal lag angle of the Solar System\'s planetary satellites. A new formulation of the tidal creep theory was proposed in Folonier et al. (2018). The new version of the theory leads to a consistent treatment of the rotational dynamics of the tidally deformed body, where forced librations around the synchronous solution (which are characteristic in the case of rigid bodies such as super-Earths and planetary satellites) are reproduced. Furthermore, the new version of the tidal creep theory allows a study of the equilibrium figure of the tidal deformed body in a much simpler way than the previous version of the theory. In this thesis, we present applications of the tidal creep theory to several cases, where both gas giant planets and Earth-like rigid planets are considered. We also discuss in detail the differences between the first version of the creep tide theory (see Ferraz-Mello 2013, 2015) and the new version (see Folonier et al. 2018). |
publishDate |
2022 |
dc.date.issued.fl_str_mv |
2022-05-06 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/doctoralThesis |
format |
doctoralThesis |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://doi.org/10.11606/T.14.2022.tde-20062022-170909 |
url |
https://doi.org/10.11606/T.14.2022.tde-20062022-170909 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
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openAccess |
dc.publisher.none.fl_str_mv |
Universidade de São Paulo |
dc.publisher.program.fl_str_mv |
Astronomia |
dc.publisher.initials.fl_str_mv |
USP |
dc.publisher.country.fl_str_mv |
BR |
publisher.none.fl_str_mv |
Universidade de São Paulo |
dc.source.none.fl_str_mv |
reponame:Biblioteca Digital de Teses e Dissertações da USP instname:Universidade de São Paulo (USP) instacron:USP |
instname_str |
Universidade de São Paulo (USP) |
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USP |
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USP |
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Biblioteca Digital de Teses e Dissertações da USP |
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Biblioteca Digital de Teses e Dissertações da USP |
repository.name.fl_str_mv |
Biblioteca Digital de Teses e Dissertações da USP - Universidade de São Paulo (USP) |
repository.mail.fl_str_mv |
virginia@if.usp.br|| atendimento@aguia.usp.br||virginia@if.usp.br |
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1794502890586374144 |