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Earth’s magnetosphere and outer radiation belt under sub-Alfvénic solar wind

机译:亚Alfvénic太阳风下的地球磁层和外部辐射带

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The interaction between Earth’s magnetic field and the solar wind results in the formation of a collisionless bow shock 60,000–100,000?km upstream of our planet, as long as the solar wind fast magnetosonic Mach (hereafter Mach) number exceeds unity. Here, we present one of those extremely rare instances, when the solar wind Mach number reached steady values <1 for several hours on 17 January 2013. Simultaneous measurements by more than ten spacecraft in the near-Earth environment reveal the evanescence of the bow shock, the sunward motion of the magnetopause and the extremely rapid and intense loss of electrons in the outer radiation belt. This study allows us to directly observe the state of the inner magnetosphere, including the radiation belts during a type of solar wind-magnetosphere coupling which is unusual for planets in our solar system but may be common for close-in extrasolar planets.
机译:只要太阳风快速磁控马赫数(以下称马赫数)超过1,地球磁场与太阳风之间的相互作用就会在我们的星球上游形成60,000–100,000?km的无碰撞弓形冲击。在这里,我们介绍了一种极为罕见的情况,2013年1月17日数小时的太阳风马赫数达到稳定值<1时。近地环境中十多艘航天器的同时测量显示了弓形冲击的消逝,磁层顶的向阳运动以及外部辐射带中电子的极快速而强烈的损失。这项研究使我们能够直接观察内部磁层的状态,包括在太阳风-磁层耦合类型期间的辐射带,这对于我们太阳系中的行星是不常见的,但对于太阳系外行星而言可能很常见。

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