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Solar wind-magnetosphere energy coupling function fitting: Results froma global MHD simulation

机译:太阳风-磁层能量耦合函数拟合:全球MHD模拟的结果

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摘要

Quantitatively estimating the energy input from the solar wind into the magnetosphere on a global scale is still an observational challenge. We perform three-dimensional magnetohydrodynamic (MHD) simulations to derive the energy coupling function. Based on 240 numerical test runs, the energy coupling function is given by E_(in) = 3.78 × 10~7n_(sw)~(0.24)V_(sw)~(1.47)B_T~(0.86) [sin~(2.70)(θ∕2) + 0.25]. We study the correlations between the energy coupling function and a wide variety of magnetospheric activity, such as the indices of Dst, Kp, ap, AE, AU, AL, the polar cap index, and the hemispheric auroral power. The results indicate that this energy coupling function gives better correlations than the ε function. This result is also applied to a storm event under northward interplanetary magnetic field conditions. About 13% of the solar wind kinetic energy is transferred into the magnetosphere and about 35% of the input energy is dissipated in the ionosphere, consistent with previous studies.
机译:在全球范围内定量估计从太阳风到磁层的能量输入仍然是一个观察难题。我们执行三维磁流体动力学(MHD)模拟以得出能量耦合函数。基于240个数值试验,能量耦合函数为E_(in)= 3.78×10〜7n_(sw)〜(0.24)V_(sw)〜(1.47)B_T〜(0.86)[sin〜(2.70) (θ∕ 2)+ 0.25]。我们研究了能量耦合函数与各种磁层活动之间的相关性,如Dst,Kp,ap,AE,AU,AL,极冠指数和半球极光功率。结果表明,该能量耦合函数比ε函数具有更好的相关性。此结果也适用于北向行星际磁场条件下的暴风雨事件。与以前的研究一致,大约13%的太阳风动能被转移到磁层中,而大约35%的输入能量被耗散在电离层中。

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