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首页> 外文期刊>The Astrophysical journal >MONITORING SHORT-TERM COSMIC-RAY SPECTRAL VARIATIONS USING NEUTRON MONITOR TIME-DELAY MEASUREMENTS
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MONITORING SHORT-TERM COSMIC-RAY SPECTRAL VARIATIONS USING NEUTRON MONITOR TIME-DELAY MEASUREMENTS

机译:使用中子监测仪时延测量来监测短期宇宙射线光谱变化

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摘要

Neutron monitors (NMs) are ground-based detectors of cosmic-ray showers that are widely used for high-precision monitoring of changes in the Galactic cosmic-ray (GCR) flux due to solar storms and solar wind variations. In the present work, we show that a single neutron monitor station can also monitor short-term changes in the GCR spectrum, avoiding the systematic uncertainties in comparing data from different stations, by means of NM time-delay histograms. Using data for 2007–2014 from the Princess Sirindhorn Neutron Monitor, a station at Doi Inthanon, Thailand, with the world's highest vertical geomagnetic cutoff rigidity of 16.8 GV, we have developed an analysis of time-delay histograms that removes the chance coincidences that can dominate conventional measures of multiplicity. We infer the "leader fraction" L of neutron counts that do not follow a previous neutron count in the same counter from the same atmospheric secondary, which is inversely related to the actual multiplicity and increases for increasing GCR spectral index. After correction for atmospheric pressure and water vapor, we find that L indicates substantial short-term GCR spectral hardening during some but not all Forbush decreases in GCR flux due to solar storms. Such spectral data from Doi Inthanon provide information about cosmic-ray energies beyond the Earth's maximum geomagnetic cutoff, extending the reach of the worldwide NM network and opening a new avenue in the study of short-term GCR decreases.
机译:中子监测器(NMs)是宇宙射线阵雨的地面探测器,广泛用于高精度监测由于太阳风暴和太阳风的变化而产生的银河系宇宙射线(GCR)通量的变化。在目前的工作中,我们表明,单个中子监测站还可以监测GCR频谱的短期变化,从而通过NM时延直方图避免了比较来自不同站的数据时的系统不确定性。利用泰国Doi Inthanon的Sirirhornhorn中子监测器公主站2007-2014年的数据,该站的垂直地磁截止刚度为世界最高,为16.8 GV,我们对时延直方图进行了分析,从而消除了主导了传统的多元化措施。我们从相同的大气次级推断出在相同计数器中不遵循先前中子计数的中子计数的“前导分数” L,这与实际多重性成反比,并且随着GCR光谱指数的增加而增加。对大气压力和水蒸气进行校正后,我们发现L表示在部分但并非全部Forbush因太阳风暴导致的GCR通量下降期间,短期GCR光谱出现了实质性硬化。来自茵他侬山的光谱数据提供了有关宇宙射线能量的信息,这些能量超出了地球的最大地磁截止范围,扩展了全球NM网络的覆盖范围,并为研究短期GCR下降开辟了新途径。
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