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arXiv 2502.01302astro-ph.EPastro-ph.SRphysics.geo-ph
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动力学潮汐与轨道运动的耦合

Coupling of dynamical tide and orbital motion

Xing Wei

AI总结:

本文使用二维浅水模型测试动力学潮汐与轨道运动的耦合,发现该耦合使潮汐耗散随轨道间距增大而增加,在研究长期轨道演化时不可忽略。

摘要:

动力学潮汐由能与轨道运动产生共振的各种波组成。我们使用可应用于覆盖薄层海洋或大气的岩石行星的简单二维浅水模型,测试了这种动力学潮汐与轨道运动的耦合。随后,我们将地月系统作为基准模型来计算潮汐共振与轨道演化。我们发现,由于动力学潮汐与轨道运动的耦合,潮汐耗散甚至可随轨道间距的增大而增加。我们得出结论,在研究长期时间尺度上的轨道演化时,该耦合是不可忽略的。

英文摘要:

Dynamical tide consists of various waves that can resonate with orbital motion. We test this coupling of dynamical tide and orbital motion using a simple two-dimensional shallow water model, which can be applied to a rocky planet covered with thin ocean or atmosphere. Then we take the earth-moon system as a fiducial model to calculate the tidal resonances and orbital evolution. We find that tidal dissipation can even increase with increasing orbital separation because of the coupling of dynamical tide and orbital motion. We draw the conclusion that the coupling is not negligible to study the orbital evolution on secular timescale.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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