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Solar cycle dependence of the diurnal anisotropy of 0.6 TeV cosmic ray intensity observed with the Matsushiro underground muon detector

机译:太阳周期依赖于0.6 TeV宇宙射线的日变化各向异性   用matsushiro地下μ子探测器观察到的强度

摘要

We analyze the temporal variation of the diurnal anisotropy of sub-TeV cosmicray intensity observed with the Matsushiro (Japan) underground muon detectorover two full solar activity cycles in 1985-2008. The average siderealamplitude over the entire period is 0.034+-0.003 %, which is roughly one thirdof the amplitude reported from AS and deep-underground muon experimentsmonitoring multi-TeV GCR intensity suggesting a significant attenuation of theanisotropy due to the solar modulation. We find, on the other hand, only weakcorrelations either with the solar activity- or magnetic-cycles. We examine thetemporal variation of the "single-band valley depth" (SBVD) quoted by theMilagro experiment and, by contrast with recent Milagro reports, we find nosteady increase in the Matsushiro observations in a 7-year period between 2000and 2007. We suggest, therefore, that the steady increase of the SBVD reportedby the Milagro experiment is not caused by the decreasing solar modulation inthe declining phase of the 23rd solar activity cycle.
机译:我们分析了在1985-2008年两个松散的太阳活动周期中,用松代(日本)地下μ子探测器观测到的亚TeV宇宙射线强度的日各向异性的时间变化。整个期间的平均副振幅为0.034 + -0.003%,大约是AS和监测多TeV GCR强度的深地下μ子实验报告的振幅的三分之一,这表明由于太阳调制,各向异性明显减弱。另一方面,我们发现只有与太阳活动或磁循环的弱相关性。我们研究了米拉格罗实验所引用的“单带谷深”(SBVD)的时间变化,并且与最近的米拉格罗报告相反,我们发现在2000年至2007年的7年中,松代观测的观测值并没有稳定增长。我们建议,因此,由Milagro实验报告的SBVD的稳定增加并不是由第23个太阳活动周期下降阶段的太阳调制下降引起的。

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