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Physics-based solar wind driver functions for the magnetosphere: Combining the reconnection-coupled MHD generator with the viscous interaction

机译:基于物理的太阳风驱动器对磁层的功能:将重新连接的MHD发电机与粘性相互作用相结合

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[1] Driver functions for the Earth's magnetosphere-ionosphere system are derived from physical principles. Two processes act simultaneously: a reconnection-coupled MHD generator G and a viscous interaction. G accounts for the dayside reconnection rate, the length of the reconnection X line, and current saturation limits for the solar wind generator. Two viscous drivers are derived: Bohm viscosity B and the freestream-turbulence effect F. A problematic proxy effect is uncovered wherein the viscous driver functions also describe the strength of reconnection. Two magnetospheric-driver functions written in terms of upstream solar wind parameters are constructed: G + B and G + F. The driver functions are tested against seven geomagnetic indices. The reaction of the geomagnetic indices to G + B and G + F is nonlinear: Nonlinear versions of the driver functions are supplied. Applying the driver functions at multiple time steps yields correlation coefficients of ~85% with the AE and K_p indices; it is argued that multiple time stepping removes high-frequency uncorrelated signal from the drivers. Autocorrelation-function analysis shows strong 1 day and 1 year periodicities in the AE index, which are not in the solar wind driver functions; correspondingly, high-pass and low-pass filtering finds uncorrelated signal at 1 day and 1 year timescales. Residuals (unpredicted variance) between the geomagnetic indices and the driver functions are analyzed: The residuals are anticorrelated with the solar wind velocity, the solar F_(10.7) radio flux, and the solar wind current saturation parameter. Removing diurnal, semiannual, and annual trends from the indices improves their correlation with the solar wind driver functions. Simplified versions of the driver functions are constructed: The simplified drivers perform approximately as well as the full drivers.
机译:[1]地球磁电离层系统的驱动程序功能是从物理原理得出的。两个过程同时起作用:一个重新连接的MHD发生器G和一个粘性相互作用。 G代表日间重新连接速率,重新连接X线的长度以及太阳能风力发电机的电流饱和极限。得出两个粘性驱动因子:玻姆粘度B和自由流湍流效应F。发现了一个有问题的代理效应,其中粘性驱动因子的功能也描述了重新连接的强度。构造了两个用上游太阳风参数表示的磁层驱动函数:G + B和G +F。针对七个地磁指数测试了该驱动函数。地磁指数对G + B和G + F的反应是非线性的:提供了驱动程序函数的非线性版本。在多个时间步上应用驱动程序函数会产生与AE和K_p指数相关的〜85%的相关系数;有人认为,多重时间步进可以消除驱动器产生的高频不相关信号。自相关函数分析显示AE指数具有1天和1年的强周期,而在太阳风驱动器函数中则没有。相应地,高通和低通滤波在1天和1年的时间尺度上发现了不相关的信号。分析了地磁指数和驱动函数之间的残差(不可预测的方差):残差与太阳风速,太阳F_(10.7)无线电通量和太阳风电流饱和度参数成反相关。从指数中删除日,半年度和年度趋势可改善它们与太阳风驱动器功能的相关性。构造了驱动程序功能的简化版本:简化的驱动程序的性能与完整的驱动程序差不多。

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