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arXiv 2302.00634physics.flu-dynastro-ph.SRphysics.plasm-phphysics.space-ph
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湍动磁鞘的弛豫

Relaxation of the turbulent magnetosheath

Francesco Pecora, Yan Yang, Alexandros Chasapis, Sergio Servidio, Manuel Cuesta, Sohom Roy, Rohit Chhiber, Riddhi Bandyopadhyay, D. J. Gershman, B. L. Giles, J.… 展开作者

Francesco Pecora, Yan Yang, Alexandros Chasapis, Sergio Servidio, Manuel Cuesta, Sohom Roy, Rohit Chhiber, Riddhi Bandyopadhyay, D. J. Gershman, B. L. Giles, J. L. Burch, William H. Matthaeus

AI总结:

本文首次提供了观测证据,表明在地球磁鞘这种强湍动自然环境中,湍流可通过局部弛豫形成非线性减弱、能量级联受损的局部准平衡“单元化”状态。

摘要:

在湍流中,非线性项通过所谓的能量级联驱动能量从大尺度涡旋向小尺度转移。湍流通常向最小化能量的状态弛豫;通常这些状态是在全局上被考虑的。然而,湍流也可以向局部准平衡状态弛豫,从而形成非线性强度减弱且能量级联受损的斑块或单元。我们首次展示了令人信服的观测证据,表明这种湍流的“单元化”可以在像地球磁鞘这样强湍动的自然环境中由于局部弛豫而发生。

英文摘要:

In turbulence, nonlinear terms drive energy transfer from large-scale eddies into small scales through the so-called energy cascade. Turbulence often relaxes toward states that minimize energy; typically these states are considered globally. However, turbulence can also relax toward local quasi-equilibrium states, creating patches or cells where the magnitude of nonlinearity is reduced and energy cascade is impaired. We show, for the first time, compelling observational evidence that this ``cellularization'' of turbulence can occur due to local relaxation in a strongly turbulent natural environment such as the Earth's magnetosheath.

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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