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Large and Sharp Changes of Solar Wind Dynamic Pressure and Disturbances of the Magnetospheric Magnetic Field at Geosynchronous Orbit Caused by These Variations

机译:这些变化引起的太阳风动压的大而急剧变化以及地球同步轨道上的磁层磁场的扰动

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摘要

The large and sharp changes of solar wind dynamic pressure, found from the INTERBALL-1 satellite and WIND spacecraft data, are compared with simultaneous magnetic field disturbances in the magneto-sphere measured by geosynchronous GOES-8, GOES-9, and GOES-10 satellites. For this purpose, about 200 events in the solar wind, associated with sharp changes of the dynamic pressure, were selected from the INTERBALL-1 satellite data obtained during 1996-1999. The large and sharp changes of the solar wind dynamic pressure were shown to result in rapid variations of the magnetic field strength in the outer magnetosphere, the increase (drop) of the solar wind dynamic pressure always lead to an increase (drop) of the geosynchronous magnetic field magnitude. The value of the geomagnetic field variation strongly depends on the local time of the observation point, reaching a maximum value near the noon meridian. It is shown that the direction of the B_z component of the interplanetary magnetic field has virtually no effect on the geomagnetic field variation because of a sharp jump of pressure. The time shift between an event in the solar wind and its response in the magnetosphere at a geosynchronous orbit essentially depends on the inclination of the front of a solar wind disturbance to the Sun—Earth line.
机译:从INTERBALL-1卫星和WIND航天器数据中发现的太阳风动压的巨大变化和急剧变化,与通过地球同步GOES-8,GOES-9和GOES-10测量的磁层同时磁场干扰进行了比较。卫星。为此,从1996-1999年间获得的INTERBALL-1卫星数据中选出了大约200个太阳风事件,与动态压力的急剧变化有关。结果表明,太阳风动压的急剧变化会导致外磁层磁场强度的快速变化,太阳风动压的增加(下降)总是导致地球同步的增加(下降)。磁场强度。地磁场变化的值在很大程度上取决于观测点的当地时间,在中午子午线附近达到最大值。结果表明,由于压力的急剧变化,行星际磁场的B_z分量的方向实际上对地磁场的变化没有影响。在太阳风中的事件与其在地球同步轨道上的磁层中的响应之间的时间偏移,基本上取决于太阳风扰动的前缘相对于太阳地球线的倾斜度。

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