Abstract
Inner belt proton fluxes exhibit striking multi-year modulation, driven by solar EUV variability, geomagnetic disturbances, and thermospheric density variations. Here we introduce the Solar–Terrestrial Recharge Oscillator (STRO), a reduced-order dynamical model that captures this long-term variability with only two state variables and a minimal set of simple solar–geomagnetic inputs. The model couples proton population dynamics with an effective atmospheric state controlled by a smoothed F10.7 proxy, capturing nonlinear feedback between solar forcing and trapped-particle evolution. A global parameter optimization procedure is employed in order to derive physically consistent coefficients governing accumulation, loss, and solar-driven variability. The optimized STRO model mimics the observed multi-year proton flux record with remarkable fidelity, capturing both amplitude and phase structure, as well as the dominant solar cycle-scale spectral peak. Segmented comparisons over two separate observed intervals (2014–2020 and 2020–2025) illustrate stable cycle-to-cycle performance and minimal phase bias. STRO offers a computationally efficient, interpretable alternative to high-dimensional transport models and purely empirical predictors, holding promise for long-term reconstruction, sensitivity studies, and operational space environment applications.
| Original language | English |
|---|---|
| Journal | Advances in Space Research |
| DOIs | |
| Publication status | Accepted/In press - 2025 |
Bibliographical note
Publisher Copyright:© 2025 COSPAR. Published by Elsevier B.V. All rights are reserved, including those for text and data mining, AI training, and similar technologies.
Keywords
- F10.7 index
- Nonlinear dynamical modeling
- Proton flux
- Radiation belt dynamics
- Solar EUV forcing
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