Observation and analysis of the anisotropic Forbush decrease of 24 March 2024

dc.contributor.authorMishev A.
dc.contributor.authorLarsen N.
dc.contributor.authorAsvestari E.
dc.contributor.authorSáiz A.
dc.contributor.authorShea M.A.
dc.contributor.authorStrauss D.T.
dc.contributor.authorRuffolo D.
dc.contributor.authorBanglieng C.
dc.contributor.authorSeunarine S.
dc.contributor.authorDuldig M.L.
dc.contributor.authorGil A.
dc.contributor.authorBlanco J.J.
dc.contributor.authorGarcía-Población O.
dc.contributor.authorCervino-Solana P.
dc.contributor.authorAdams J.H.
dc.contributor.authorUsoskin I.
dc.contributor.correspondenceMishev A.
dc.contributor.otherMahidol University
dc.date.accessioned2026-02-08T18:19:23Z
dc.date.available2026-02-08T18:19:23Z
dc.date.issued2025-12-30
dc.description.abstractIt is known that GCR flux exhibits notable transient suppressions due to coronal mass ejections (CMEs) and co-rotating interaction regions (CIRs) in the solar wind, called Forbush decreases (FDs). FDs are observed as fast, occasionally two-step, decreases in the count rate of particle counters. The decrease is usually followed by a gradual recovery taking up to several days or even a week. A particularly strong FD, observed as suppression of the flux of galactic cosmic rays was observed by the global network of ground-based neutron monitors (NMs) on 24–25 March 2024. The decrease revealed an unusual rapid recovery leading to false ground-level enhancement alarm from the cosmic radiation warning systems. The event was highly anisotropic, with anisotropy focused nearly on the anti-sunward direction. Here we present the observations, focusing on NM records, and the corresponding analysis.
dc.identifier.citationProceedings of Science Vol.501 (2025)
dc.identifier.doi10.22323/1.501.1333
dc.identifier.eissn18248039
dc.identifier.scopus2-s2.0-105029067930
dc.identifier.urihttps://repository.li.mahidol.ac.th/handle/123456789/114898
dc.rights.holderSCOPUS
dc.subjectMultidisciplinary
dc.titleObservation and analysis of the anisotropic Forbush decrease of 24 March 2024
dc.typeConference Paper
mu.datasource.scopushttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=105029067930&origin=inward
oaire.citation.titleProceedings of Science
oaire.citation.volume501
oairecerif.author.affiliationHelsingin Yliopisto
oairecerif.author.affiliationNagoya University
oairecerif.author.affiliationOulun Yliopisto
oairecerif.author.affiliationUniversity of Tasmania
oairecerif.author.affiliationUniversidad de Alcalá
oairecerif.author.affiliationNorth-West University
oairecerif.author.affiliationFaculty of Science, Mahidol University
oairecerif.author.affiliationSiedlce University of Natural Sciences and Humanities
oairecerif.author.affiliationRajamangala University of Technology Thanyaburi (RMUTT)
oairecerif.author.affiliationUniversity of Wisconsin-River Falls
oairecerif.author.affiliationCenter for Space Plasma and Aeronomic Research
oairecerif.author.affiliationSodankylä Geophysical Observatory

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