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Forecasting Earth's magnetopause, magnetosheath, and bow shock

机译:预测地球的磁更年期,磁震度和弓激波

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The magnetopause and bow shock are two of the most important discontinuities in near Earth space, separating three distinct plasma regimes: the solar wind, magnetosheath, and the magnetosphere. Both discontinuities are sensitive to the solar wind conditions. They change their shape and location in space in response to upstream solar wind variations. Prediction of the location of a satellite relative to these two boundaries helps satellite operators to be prepared for major changes in plasma condition. The physical conditions near the magnetopause are useful information for magnetospheric models. Over the past decades, our observational knowledge and physical understanding of these regions have been advanced significantly. We have developed the capability of prediction. The location of the magnetopause and its dependence on the upstream conditions can be relatively accurately predicted. Prediction models have been tested extensively. The success rate is extremely high and the false-alarm rate is relatively low. A magnetosheath prediction model has been developed and tested. Some of the magnetosheath quantities can often be predicted fairly accurately. Others may have slightly larger errors. Further tests and scientific investigations of the causes of these errors are under way. Our ability to predict the location of the bow shock is very limited. More research is needed.
机译:磁层顶和弓形激波是近地空间中最重要的两个不连续点,它们将三种不同的等离子体状态分开:太阳风,磁石和磁层。两个不连续点都对太阳风条件敏感。它们响应上游太阳风的变化而改变其形状和空间位置。相对于这两个边界的卫星位置的预测有助于卫星运营商为等离子体状况的重大变化做好准备。磁层顶附近的物理条件对于磁层模型是有用的信息。在过去的几十年中,我们对这些地区的观测知识和物理认识有了很大的提高。我们已经开发了预测能力。磁绝顶的位置及其对上游条件的依赖性可以相对准确地预测。预测模型已经过广泛测试。成功率极高,错误警报率相对较低。已经开发并测试了磁石预测模型。通常可以相当准确地预测某些磁石荒量。其他的则可能会有稍大的错误。正在对这些错误的原因进行进一步的测试和科学调查。我们预测弓形冲击的位置的能力非常有限。需要更多的研究。

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