Publication:
Corotating solar wind structures and recurrent trains of enhanced diurnal variation in galactic cosmic rays

dc.contributor.authorT. Yeeramen_US
dc.contributor.authorD. Ruffoloen_US
dc.contributor.authorA. Sáizen_US
dc.contributor.authorN. Kamyanen_US
dc.contributor.authorT. Nutaroen_US
dc.contributor.otherMahidol Universityen_US
dc.contributor.otherSouth Carolina Commission on Higher Educationen_US
dc.contributor.otherUbon Rajathanee Universityen_US
dc.date.accessioned2018-11-09T02:12:47Z
dc.date.available2018-11-09T02:12:47Z
dc.date.issued2014-04-01en_US
dc.description.abstractData from the Princess Sirindhorn Neutron Monitor at Doi Inthanon, Thailand, with a vertical cutoff rigidity of 16.8 GV, were utilized to determine the diurnal anisotropy (DA) of Galactic cosmic rays (GCRs) near Earth during solar minimum conditions between 2007 November and 2010 November. We identified trains of enhanced DA over several days, which often recur after a solar rotation period (27 days). By investigating solar coronal holes as identified from synoptic maps and solar wind parameters, we found that the intensity and anisotropy of cosmic rays are associated with the high-speed streams (HSSs) in the solar wind, which are in turn related to the structure and evolution of coronal holes. An enhanced DA was observed after the onset of some, but not all, HSSs. During time periods of recurrent trains, the DA was often enhanced or suppressed according to the sign of the interplanetary magnetic field B, which suggests a contribution from a mechanism involving a southward gradient in the GCR density, n, and a gradient anisotropy along B × ∇n. In one non-recurrent and one recurrent sequence, an HSS from an equatorial coronal hole was merged with that from a trailing mid-latitude extension of a polar coronal hole, and the slanted HSS structure in space with suppressed GCR density can account for the southward GCR gradient. We conclude that the gradient anisotropy is a source of temporary changes in the GCR DA under solar minimum conditions, and that the latitudinal GCR gradient can sometimes be explained by the coronal hole morphology. © 2014. The American Astronomical Society. All rights reserved..en_US
dc.identifier.citationAstrophysical Journal. Vol.784, No.2 (2014)en_US
dc.identifier.doi10.1088/0004-637X/784/2/136en_US
dc.identifier.issn15384357en_US
dc.identifier.issn0004637Xen_US
dc.identifier.other2-s2.0-84896525079en_US
dc.identifier.urihttps://repository.li.mahidol.ac.th/handle/123456789/33792
dc.rightsMahidol Universityen_US
dc.rights.holderSCOPUSen_US
dc.source.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84896525079&origin=inwarden_US
dc.subjectEarth and Planetary Sciencesen_US
dc.subjectPhysics and Astronomyen_US
dc.titleCorotating solar wind structures and recurrent trains of enhanced diurnal variation in galactic cosmic raysen_US
dc.typeArticleen_US
dspace.entity.typePublication
mu.datasource.scopushttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84896525079&origin=inwarden_US

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