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Shape, Internal Structure, Zonal Winds, and Gravitational Field of Rapidly Rotating Jupiter-Like Planets

机译:形状,内部结构,区域风和快速旋转木星类似行星的引力场

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摘要

High-precision gravitational measurements by orbiting spacecraft provide a means of probing the structures, fluid motions, and convective dynamos in the interiors of the rapidly rotating outer planets. Here, the classical theory of rotating homogeneous planets is briefly reviewed. Emphasis is placed on recent developments in theories and methods that relate internal structure and processes to their gravitational signatures. Whereas early theories usually treated the effects of interior density stratification and rotational distortion as perturbations to a spherical state, recent research is marked by a self-consistent perturbation approach in which the leading-order problem accounts exactly for rotational distortion, thereby determining the basic shape, internal structure, and gravitational field of the planet. The next-order problem, which is mathematically and physically coupled with the leading-order problem, describes the modifications caused by internal fluid motions. Although the theories and methods have general applicability, advances have been spurred by the need to have a basis for interpretation of the gravitational data for Jupiter and Saturn expected from the Juno and Cassini missions.
机译:通过轨道航天器的高精度重力测量提供了探测快速旋转外行星的内部结构,流体运动和对流发电机的方法。这里,简要回顾了旋转均匀行星的经典理论。重点是最近的理论和方法的最新发展,使内部结构和流程与其引力签名相关。虽然早期理论通常将内部密度分层和旋转畸变的影响视为球形状态的扰动,但最近的研究是由自我一致的扰动方法标记,其中前导问题账户完全用于旋转失真,从而确定基本形状,地球的内部结构和引力场。在数学和物理耦合与前导问题的下一个问题描述了由内部流体运动引起的修改。虽然理论和方法具有一般适用性,但需要提出进展,以便对Jupiter和Hemo和Cassini任务的预期预期的木星和土星的引力数据进行依据。

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