dorsal/arxiv
View SchemaObservation of the Forbush decrease on 2024 May 10, using the ALPAQUITA air-shower array at the 70-1000 GV rigidity range
| Authors | M. Anzorena, E. de la Fuente, K. Fujita, R. Garcia, Y. Hayashi, K. Hibino, N. Hotta, G. Imaizumi, Y. Katayose, C. Kato, S. Kato, T. Kawashima, K. Kawata, M. Kobayashi, S. Kobayashi, T. Koi, H. Kojima, P. Miranda, S. Mitsuishi, A. Mizuno, K. Munakata, Y. Nakamura, M. Nishizawa, Y. Noguchi, S. Ogio, M. Ohishi, M. Ohnishi, A. Oshima, M. Raljevic, H. Rivera, T. Saito, T. Sako, T. K. Sako, S. Shibata, A. Shiomi, M. Subieta, F. Sugimoto, N. Tajima, W. Takano, Y. Takeyama, M. Takita, N. Tamaki, Y. Tameda, K. Tanaka, R. Ticona, H. Tsuchiya, Y. Tsunesada, S. Udo, G. Yamagishi, Y. Yamanaka, K. Yamazaki, Y. Yokoe |
|---|---|
| Categories | |
| ArXiv ID | 2601.08154vv1 |
| URL | https://arxiv.org/abs/2601.08154 |
| License | http://creativecommons.org/licenses/by/4.0/ |
Abstract
The Andes Large area PArticle detector for Cosmic ray and Astronomy (ALPACA) is a new air-shower array experiment under construction in the Bolivian Andes, and its prototype ALPAQUITA surface array has been operating since 2023 April. In addition to the traditional $\ge$3-hit or $\ge$4-hit coincidences to trigger recording air-shower events, ALPAQUITA records the counting rates of the $\ge$1-hit and $\ge$2-hit events (Any1 and Any2, respectively). We report a successful detection of a Forbush decrease occurred on 2024 May 10 caused by a passage of an interplanetary shock formed ahead of the Interplanetary Coronal Mass Ejection. The amplitude detected in the Any1 rate is 4.26$\pm$0.33% at the median primary rigidity of 76GV which is consistent with the observations with the worldwide neutron monitor and muon detector networks. Under the assumption of a power-law rigidity spectrum, we renormalized the errors of the observed amplitude ($A_{obs}$) and fitted them as a function of the median primary rigidity ($R_{m}$) of each detector and observational method. The result $A_{obs} = (10.9\% \pm 0.9\%) \times (R_{m}/10\,GV)^{-0.55 \pm 0.07}$ exhibits a hard nature of this event. Our non-detection in the Any2 rate decrease constrains the amplitude with a 2$\sigma$ upper limit to be 0.95% at 960GV. This marginally suggests an existence of a spectral softening between 100GV and 1000GV as also suggested by the Misato underground muon detector at 145GV. Although a strong geomagnetic storm was observed during this period, we conclude it does not impact our results. Our novel technique realizes a unique coverage to study the behavior of the Forbush decreases at the highest rigidity.
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"date_created": "2026-02-17T05:53:15.098000Z",
"date_modified": "2026-02-17T05:53:15.098000Z",
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"abstract": "The Andes Large area PArticle detector for Cosmic ray and Astronomy (ALPACA) is a new air-shower array experiment under construction in the Bolivian Andes, and its prototype ALPAQUITA surface array has been operating since 2023 April. In addition to the traditional $\\ge$3-hit or $\\ge$4-hit coincidences to trigger recording air-shower events, ALPAQUITA records the counting rates of the $\\ge$1-hit and $\\ge$2-hit events (Any1 and Any2, respectively). We report a successful detection of a Forbush decrease occurred on 2024 May 10 caused by a passage of an interplanetary shock formed ahead of the Interplanetary Coronal Mass Ejection. The amplitude detected in the Any1 rate is 4.26$\\pm$0.33% at the median primary rigidity of 76GV which is consistent with the observations with the worldwide neutron monitor and muon detector networks. Under the assumption of a power-law rigidity spectrum, we renormalized the errors of the observed amplitude ($A_{obs}$) and fitted them as a function of the median primary rigidity ($R_{m}$) of each detector and observational method. The result $A_{obs} = (10.9\\% \\pm 0.9\\%) \\times (R_{m}/10\\,GV)^{-0.55 \\pm 0.07}$ exhibits a hard nature of this event. Our non-detection in the Any2 rate decrease constrains the amplitude with a 2$\\sigma$ upper limit to be 0.95% at 960GV. This marginally suggests an existence of a spectral softening between 100GV and 1000GV as also suggested by the Misato underground muon detector at 145GV. Although a strong geomagnetic storm was observed during this period, we conclude it does not impact our results. Our novel technique realizes a unique coverage to study the behavior of the Forbush decreases at the highest rigidity.",
"arxiv_id": "2601.08154",
"authors": [
"M. Anzorena",
"E. de la Fuente",
"K. Fujita",
"R. Garcia",
"Y. Hayashi",
"K. Hibino",
"N. Hotta",
"G. Imaizumi",
"Y. Katayose",
"C. Kato",
"S. Kato",
"T. Kawashima",
"K. Kawata",
"M. Kobayashi",
"S. Kobayashi",
"T. Koi",
"H. Kojima",
"P. Miranda",
"S. Mitsuishi",
"A. Mizuno",
"K. Munakata",
"Y. Nakamura",
"M. Nishizawa",
"Y. Noguchi",
"S. Ogio",
"M. Ohishi",
"M. Ohnishi",
"A. Oshima",
"M. Raljevic",
"H. Rivera",
"T. Saito",
"T. Sako",
"T. K. Sako",
"S. Shibata",
"A. Shiomi",
"M. Subieta",
"F. Sugimoto",
"N. Tajima",
"W. Takano",
"Y. Takeyama",
"M. Takita",
"N. Tamaki",
"Y. Tameda",
"K. Tanaka",
"R. Ticona",
"H. Tsuchiya",
"Y. Tsunesada",
"S. Udo",
"G. Yamagishi",
"Y. Yamanaka",
"K. Yamazaki",
"Y. Yokoe"
],
"categories": [
"astro-ph.HE",
"astro-ph.SR"
],
"license": "http://creativecommons.org/licenses/by/4.0/",
"title": "Observation of the Forbush decrease on 2024 May 10, using the ALPAQUITA air-shower array at the 70-1000 GV rigidity range",
"url": "https://arxiv.org/abs/2601.08154",
"version": "v1"
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