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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:松代地下μ子探测器观测到的0.6 TeV宇宙线强度的日各向异性对太阳周期的依赖性

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We analyze the temporal variation of the solar and sidereal diurnal anisotropies of sub-TeV cosmic ray intensity observed with the Matsushiro (Japan) underground muon detector over two full solar activity cycles in 1985-2008. We find an anisotropy component in the solar diurnal anisotropy superimposed on the Compton-Getting anisotropy due to the earth’s orbital motion around the sun. The phase of this additional anisotropy is almost constant at 15:00 local solar time corresponding to the direction perpendicular to the average interplanetary magnetic field at the earth’s orbit, while the amplitude varies between a maximum (0.043±0.002 %) and minimum (0.008±0.002 %) in a clear correlation with the solar activity. The average amplitude of the sidereal diurnal variation over the entire period is 0.034±0.003 %, which is roughly one third of the amplitude reported from AS and deep-underground muon experiments monitoring multi-TeV GCR intensity, suggesting a significant attenuation of the anisotropy due to the solar modulation. We find, on the other hand, only a weak positive correlation between the sidereal diurnal anisotropy and the solar activity cycle, in which the amplitude in the “active” solar activity epoch is about twice the amplitude in the “quiet” solar activity epoch. This implies that only one fourth of the total attenuation varies in correlation with the solar activity cycle and/or the solar magnetic cycle. We finally examine the temporal variation of the “single-band valley depth” (SBVD) quoted by the Milagro experiment and, by contrast with recent Milagro’s report, we find no steady increase in the Matsushiro observations in a 7-year period between 2000 and 2007. No steady increase is observed by the Tibet air shower experiment monitoring multi-TeV GCR intensity, either. We suggest, therefore, that the steady increase of the SBVD reported by the Milagro experiment is not caused by the decreasing solar modulation in the 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宇宙射线强度的太阳和恒星日各向异性的时间变化。由于地球绕太阳公转,我们发现太阳日各向异性中的一个各向异性分量叠加在Compton-Getting各向异性上。该附加各向异性的相位在当地太阳时间15:00几乎恒定,该时间对应于垂直于地球轨道上平均行星际磁场的方向,而振幅在最大值(0.043±0.002%)和最小值(0.008±)之间变化0.002%)与太阳活动有明显的相关性。在整个周期中,恒星日变化的平均幅度为0.034±0.003%,大约是AS和监测多重TeV GCR强度的深层μ子实验报告的幅度的三分之一,表明各向异性的显着衰减是由于对太阳的调制。另一方面,我们发现恒星昼夜各向异性与太阳活动周期之间只有很小的正相关,其中“活跃”太阳活动时期的振幅大约是“安静”太阳活动时期的振幅的两倍。这意味着总衰减中只有四分之一与太阳活动周期和/或太阳磁周期相关。我们最终检查了米拉格罗实验引用的“单带谷深”(SBVD)的时间变化,并且与最近的米拉格罗的报告相反,我们发现在2000年至2000年的7年中,松代观测的观测值并没有稳定增加。 2007年。西藏空气淋浴实验监测的多TeV GCR强度也没有稳定增长。因此,我们建议,由Milagro实验报告的SBVD的稳定增加并非由第23个太阳活动周期下降阶段的太阳调制下降引起。

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