Publication:
Tracking Cosmic-Ray Spectral Variation during 2007-2018 Using Neutron Monitor Time-delay Measurements

dc.contributor.authorC. Bangliengen_US
dc.contributor.authorH. Janthaloeten_US
dc.contributor.authorD. Ruffoloen_US
dc.contributor.authorA. Sáizen_US
dc.contributor.authorW. Mitthumsirien_US
dc.contributor.authorP. Muanghaen_US
dc.contributor.authorP. Evensonen_US
dc.contributor.authorT. Nutaroen_US
dc.contributor.authorR. Pyleen_US
dc.contributor.authorS. Seunarineen_US
dc.contributor.authorJ. Madsenen_US
dc.contributor.authorP. S. Mangearden_US
dc.contributor.authorR. Macatangayen_US
dc.contributor.otherUniversity of Wisconsin-River Fallsen_US
dc.contributor.otherUbon Rajathanee Universityen_US
dc.contributor.otherMahidol Universityen_US
dc.contributor.otherThe Bartol Research Instituteen_US
dc.contributor.otherPyle Consulting Group, Inc.en_US
dc.contributor.otherNational Astronomical Research Institute of Thailanden_US
dc.date.accessioned2020-05-05T05:19:33Z
dc.date.available2020-05-05T05:19:33Z
dc.date.issued2020-02-10en_US
dc.description.abstract© 2020. The American Astronomical Society. All rights reserved.. The energy spectrum of Galactic cosmic-ray (GCR) ions at Earth varies with solar activity as these ions cross the heliosphere. Thus, this "solar modulation" of GCRs provides remote sensing of heliospheric conditions throughout the ∼11 yr sunspot cycle and ∼22 yr solar magnetic cycle. A neutron monitor (NM) is a stable ground-based detector that measures cosmic-ray rate variations above a geomagnetic or atmospheric cutoff rigidity with high precision (∼0.1%) over such timescales. Furthermore, we developed electronics and analysis techniques to indicate variations in the cosmic-ray spectral index using neutron time-delay data from a single station. Here we study solar modulation using neutron time-delay histograms from two high-altitude NM stations: (1) the Princess Sirindhorn Neutron Monitor at Doi Inthanon, Thailand, with the world's highest vertical geomagnetic cutoff rigidity, 16.7 GV, from 2007 December to 2018 April; and (2) the South Pole NM, with an atmosphere-limited cutoff of ∼1 GV, from 2013 December to 2018 April. From these histograms, we extract the leader fraction L, i.e., inverse neutron multiplicity, as a proxy of a GCR spectral index above the cutoff. After correction for pressure and precipitable water vapor variations, we find that L roughly correlates with the count rate but also exhibits hysteresis, implying a change in spectral shape after a solar magnetic polarity reversal. Spectral variations due to Forbush decreases, 27 day variations, and a ground-level enhancement are also indicated. These methods enhance the high-precision GCR spectral information from the worldwide NM network and extend it to higher rigidity.en_US
dc.identifier.citationAstrophysical Journal. Vol.890, No.1 (2020)en_US
dc.identifier.doi10.3847/1538-4357/ab6661en_US
dc.identifier.issn15384357en_US
dc.identifier.issn0004637Xen_US
dc.identifier.other2-s2.0-85082435139en_US
dc.identifier.urihttps://repository.li.mahidol.ac.th/handle/123456789/54539
dc.rightsMahidol Universityen_US
dc.rights.holderSCOPUSen_US
dc.source.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85082435139&origin=inwarden_US
dc.subjectEarth and Planetary Sciencesen_US
dc.subjectPhysics and Astronomyen_US
dc.titleTracking Cosmic-Ray Spectral Variation during 2007-2018 Using Neutron Monitor Time-delay Measurementsen_US
dc.typeArticleen_US
dspace.entity.typePublication
mu.datasource.scopushttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85082435139&origin=inwarden_US

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