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arXiv 0910.3233astro-ph.SR
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磁-重力波在太阳色球层的反射和转换:高层大气的窗口

Reflection and Conversion of Magneto-Gravity Waves in the Solar Chromosphere: Windows to the Upper Atmosphere

Marie Newington, Paul Cally

摘要:

Straus等人最近报道了在太阳色球层底部探测到向上传播的内部重力波,他假设这些可以有效地耦合到磁性区域中的阿尔芬波。这在将能量输送到更高水平方面可能是重要的。在这里,我们探讨了线性重力波在VAL C大气中的传播,反射和模式转换,并发现即使是弱磁场通常反射回重力波向下慢磁声波以及之前,他们到达阿尔芬/声学均分高度,在模式转换可能发生。然而,对于其中重力波设法在均分水平附近穿透或穿过均分水平的某些高度倾斜的磁场取向,可以存在向上行阿尔芬波和声波中的任一个或两者的实质性转换。预计波能通量与色球辐射损失相当。

英文摘要:

The detection of upward propagating internal gravity waves at the base of the Sun's chromosphere has recently been reported by Straus et al., who postulated that these may efficiently couple to Alfven waves in magnetic regions. This may be important in transporting energy to higher levels. Here we explore the propagation, reflection and mode conversion of linear gravity waves in a VAL C atmosphere, and find that even weak magnetic fields usually reflect gravity waves back downward as slow magnetoacoustic waves well before they reach the Alfven/acoustic equipartition height at which mode conversion might occur. However, for certain highly inclined magnetic field orientations in which the gravity waves manage to penetrate near or through the equipartition level, there can be substantial conversion to either or both upgoing Alfven and acoustic waves. Wave energy fluxes comparable to the chromospheric radiative losses are expected.

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