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Role of Kinetic Alfven wave and whistler wave in magnetopause reconnection region turbulence generation

机译:动力学Alfven波和吹口哨波在磁更年期重新连接区湍流产生中的作用

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In literature several studies of turbulence have been carried out based upon Kinetic Alfven waves (KAWs) and whistler wave, which lead to energy transport at a smaller scale and explained turbulent spectrum. Using cluster data, Chaston et al. 2008 have proposed wave modes physics and scaling in the magnetopause region. However, KAWs and whistler waves are also observed in the vicinity of x-line in reconnection site in magnetopause. Therefore, we have proposed a model to study the evolution of nonlinear (coherent) structures and turbulence generation by taking the powerful KAWs but weak whistler in magnetic reconnection site. For this study the dynamical evolution equations are derived by taking into account the ponderomotive force driven density modification and magnetic field fluctuations due to shear field modelled by the Harris sheet. Further, governing equations have been solved numerically for magnetopause region parameters. Also, a semi-analytical model has also been developed to estimate the scale sizes of coherent structures. For numerical integrations we have used the pseudospectral method and finite difference method and for semi-analytically Runge Kutta method. Simulated results have shown the evolution of coherent structures or current sheets, which are capable to energy transfer efficiently. These structures have scale size around ion gyroradius as well as electron inertial length as calculated analytically. At a later time the chaotic structures arise in this reconnection site. This gives the signature of turbulence generation. Therefore, the corresponding power spectrum is also evaluated and compared with observational Cluster data based spectra reported by, Chaston et al., 2008 and Matteini et al., 2017. Based on the present model, we conclude that the role of KAWs and Whistler waves in the turbulence generation and reconnection site is very important.
机译:在文献中,已经基于动力学Alfven波(KAW)和惠斯勒波进行了一些湍流研究,这导致了较小尺度的能量传输并解释了湍流谱。使用群集数据,Chaston等。 2008年提出了在磁更年期地区的波模式物理和定标。然而,在绝经期重新连接部位的x线附近也观察到KAW和哨声波。因此,我们提出了一个模型来研究非线性(相干)结构的演变和湍流产生,方法是在磁重联部位采用强大的KAW而弱的啸叫声。在本研究中,通过考虑由重动力驱动的密度修正和由于哈里斯工作表建模的剪切场而引起的磁场波动,得出了动力学演化方程。此外,对于磁更年期区域参数,已经用数值方法求解了控制方程。此外,还开发了一个半分析模型来估计相干结构的尺度大小。对于数值积分,我们使用了伪光谱法和有限差分法,对于半解析性的Runge Kutta方法。仿真结果显示了能够有效传递能量的相干结构或电流表的演变。这些结构具有围绕离子陀螺半径的尺度尺寸以及通过分析计算得出的电子惯性长度。在稍后的时间,在该重新连接部位中出现了混沌结构。这给出了湍流产生的特征。因此,还对相应的功率谱进行了评估,并与Chaston等人,2008年和Matteini等人,2017年报告的基于观测聚类数据的谱进行了比较。基于当前模型,我们得出结论,KAW和惠斯勒波的作用在湍流产生和重新连接的部位非常重要。

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