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arXiv 0810.1706astro-ph
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关于220.7信号的太阳起源

On the solar origin of the 220.7 signal

A. Jimenez, R. A. Garcia

摘要:

在过去的几十年里,人们对太阳的引力模进行了长期的研究。Garcia等人(2007年)利用它们的渐近性质,通过分析GOLF/SoHO仪器获得的速度功率谱的25和140 muHz之间的频谱窗口,发现了偶极g模式的特征。利用这一结果,可以检查太阳内部结构的一些特性(Garcia,Mathur & Ballot 2008)以及核心动力学的一些迹象。然而,对这种模式的单独检测仍然是难以捉摸的,它们需要真正提高我们对太阳最深层的了解(Mathur等人,2008)。在这项工作中,我们研究的信号在220.7 μ Hz,这是目前在过去10年中的大多数日震仪器。该信号先前已被确定为GOLF数据(Turck-Chieze等人,2004; Mathur等人,2007)和SPM/VIRGO(Garcia等人,2008)中g模式候选的一部分,置信水平超过90%。它可以被标记为l= 2n =-3g模式,因为它在预期该模式的区域中。我们已经检查了220.7 muHz信号可能有一个仪器的起源没有成功的可能性,通过分析所有可用的内务数据,以及滚动,髓和偏航的SoHO航天器的信息。因此,我们相信这个信号来自太阳。

英文摘要:

Gravity modes in the Sun have been long searched during the past decades. Using their asymptotic properties Garcia et al. (2007) found the signature of the dipole g modes analyzing an spectral window between 25 and 140 muHz of velocity power spectrum obtained from the GOLF/SoHO instrument. Using this result it has been possible to check some properties of the structure of the solar interior (Garcia, Mathur & Ballot 2008) as well as some indications on the dynamics of the core. However, the individual detection of such modes remains evasive and they are needed to really improve our knowledge of the deepest layers in the Sun (Mathur et al. 2008). In this work we study the signal at 220.7 muHz which is present in most of the helioseismic instruments during the last 10 years. This signal has been previously identified as part of a g-mode candidate in the GOLF data (Turck-Chieze et al. 2004; Mathur et al. 2007) and in SPM/VIRGO (Garcia et al. 2008) with more than 90% confidence level. It could be labelled as the l=2 n=-3 g mode as it is in the region were this mode is expected. We have checked the possibility that the 220.7 muHz signal could have an instrumental origin without success by analysing all the available housekeeping data as well as the information on the roll, pith and yaw of the SoHO spacecraft. In consequence, we are confident that this signal has a solar origin.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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