Charge-sign dependent drift effects in the time-lag of cosmic-ray variation relative to solar activity observed with CALET

Author/Creator ORCID

Department

Program

Citation of Original Publication

Adriani, O., Y. Akaike, K. Asano, et al. “Charge-Sign Dependent Drift Effects in the Time-Lag of Cosmic-Ray Variation Relative to Solar Activity Observed with CALET.” Progress of Theoretical and Experimental Physics, February 17, 2026, ptag025. https://doi.org/10.1093/ptep/ptag025.

Rights

This work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
Public Domain

Subjects

Abstract

The 11-yr variation of galactic cosmic-ray flux lags behind the variation of the sunspot number. An average ∼1-yr time-lag is expected from the outward propagating solar wind with the frozen-in photospheric magnetic field varying in the solar cycle, and from the inward diffusive transport of cosmic-ray particles. The long-term neutron monitor data, however, show that the time-lag is significantly longer (shorter) in the odd (even) solar cycle. In this paper, we analyze the time-lag in proton and electron fluxes observed by the Calorimetric Electron Telescope (CALET). It is found that the time-lag is similar in proton and electron fluxes during an A > 0 polarity epoch of the solar dipole magnetic field. In an even solar cycle 24 including a polarity reversal from A < 0 to A > 0, on the other hand, it is found that the time-lag of proton (electron) flux variation is significantly shorter (longer) than the average ∼1-yr lag by analyzing the combined data with CALET and AMS-02. This is the first observation of the charge-sign dependent time-lag. We demonstrate that these observations can be qualitatively interpreted in terms of different 11-yr time profiles of proton and electron fluxes in A > 0 and A < 0 epochs expected from the drift effect.