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Effects of dipole tilt angle on geomagnetic activity

机译:偶极子倾角对地磁活动的影响

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The relationship between the orientation of the interplanetary magnetic field (IMF), represented by the clock angle which is the angle denned by 1MF-B_y and -B_z components, and the AL and AU indices is examined at various dipole tilt angles for the period of 1978-1988. We use the IMF data obtained from the IMP 8 satellite, AL and AU indices with corrected seasonal variations, and the dipole tilt angle, which is the dipole magnetic latitude of the subsolar point calculated as a function of the day of year and universal time. For both positive (dipole tilted to the Sun) and negative dipole tilt angles, the values of |AL| and AU decrease as the IMF clock angle moves away from 180, becoming more northward. The indices also tend to become smaller for larger dipole tilt angle, either toward or away from the Sun. This dependence on dipole tilt angle enhances the semiannual variation of geomagnetic activity.
机译:在不同的偶极倾斜角下,检查了以1MF-B_y和-B_z分量定义的角度即时钟角表示的行星际磁场(IMF)的方向与AL和AU指数之间的关系。 1978年至1988年。我们使用从IMP 8卫星获得的IMF数据,经校正的季节性变化的AL和AU指数,以及偶极子倾斜角,即根据一年中的某天和世界时间计算的次太阳点的偶极子磁纬度。对于正(偶极向太阳倾斜)和负偶极倾斜角,| AL |的值随着IMF时钟角从180度移向北,AU减小。对于较大的偶极子倾斜角,朝向或远离太阳的折射率也趋于变小。这种对偶极子倾斜角的依赖性增强了地磁活动的半年变化。

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