Simulating stellar coronal rain and slingshot prominences

Simon Daley-Yates, Moira Jardine
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Abstract

We have numerically demonstrated that simulated cool star coronae naturally form condensations. If the star rotates slowly, with a co-rotation radius greater than the Alfv\'{e}n radius (i.e. $R_{\mathrm{K}} > R_{\mathrm{A}}$), these condensations will form below the co-rotation radius $R_{\mathrm{K}}$ and simply fall back to the stellar surface as coronal rain. If, however, the star is more rapidly rotating, ($R_{\mathrm{K}} < R_{\mathrm{A}}$), not only rain will form but also ``slingshot prominences''. In this case, condensations collect into a large mass reservoir around the co-rotation radius, from which periodic centrifugal ejections occur. In this case, some $51\%$ of the coronal mass is cold gas, either in rain or prominences. We find that 21\% of the mass lost by our simulated fast rotating star is cold gas. Studies of stellar mass-loss from the hot wind do not consider this component of the wind and therefore systematically underestimate mass-loss rates of these stars. Centrifugal ejections happen periodically, between every 7.5 - 17.5 hours with masses clustering around $10^{16}$ g, These results agree well with observational statistics. Contrasting the fast and slow rotating magnetospheres, we find that there are two distinct types of solutions, high lying and low lying loops. Low lying loops only produce coronal rain whereas high lying loops produce both rain and slingshots.
模拟恒星日冕雨和弹弓状突出物
我们用数值方法证明,模拟的冷恒星日冕会自然形成凝聚。如果恒星旋转缓慢,共转半径大于Alfv\'{e}n 半径(即$R_{\mathrm{K}} > R_{\mathrm{A}}$),这些凝聚体就会在共转半径$R_{\mathrm{K}}$下方形成,并以日冕雨的形式简单地落回恒星表面。然而,如果恒星的自转速度更快($R_{mathrm{K}} < R_{mathrm{A}}$),那么不仅会形成日冕雨,还会形成 "弹射状突出"。在这种情况下,冷凝物会在同向旋转半径周围聚集成一个巨大的质量库,并从中发生周期性的离心喷射。在这种情况下,日冕质量中有51%是冷气体,要么是雨,要么是突出物。我们发现,我们模拟的快速旋转恒星损失的质量中有21%是冷气体。离心喷射是周期性的,每7.5-17.5小时发生一次,质量聚集在10^{16}$ g左右,这些结果与观测统计数据非常吻合。对比快速旋转和慢速旋转的磁层,我们发现有两种不同类型的解决方案:高位环和低位环。低平环只产生日冕雨,而高平环同时产生日冕雨和弹弓。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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