Real-time prediction of geomagnetic storms using Solar Orbiter as a far upstream solar wind monitor
Emma E. Davies, Eva Weiler, Christian Möstl, Satabdwa Majumdar, Hannah T. Rüdisser, Timothy S. Horbury, Helen O'Brien, Jean Morris, Alastair Crabtree
TL;DR
This work demonstrates the feasibility of real-time CME forecasting using Solar Orbiter as a far-upstream monitor, delivering actionable lead times for geomagnetic impact by combining (i) ELEvo-based arrival predictions constrained by upstream in situ data, (ii) magnetic-field scaling and temporal stretching to predict the L1 field, and (iii) the Temerin & Li geomagnetic model to forecast SYM-H with ensemble uncertainty. The two March 2024 CME events show that upstream measurements can reproduce near-Earth magnetic structure and yield substantial lead times (up to ~34 hours before storm peaks), though arrival-time errors remain several hours and magnitude predictions can be limited by missing plasma data and complex CME evolution. Key insights include the dominance of radial evolution over longitudinal differences at separations up to ~10°, the value of using simple, observation-constrained propagation schemes, and the substantial benefit of continuous upstream plasma and field measurements for improving forecast reliability. The results support the strategic value of future dedicated upstream missions and data assimilation for enhanced space weather prediction and preparedness.
Abstract
We present the first real-time predictions of coronal mass ejection (CME) magnetic structure and resulting geomagnetic impact at Earth for two events using far-upstream observations from Solar Orbiter during March 2024. While our approach assumes idealized conditions for CME propagation and scaling, in situ magnetic field data from upstream monitors still produced realistic predictions despite the large heliocentric distance between Solar Orbiter and L1 (0.53 and 0.60 au). Geomagnetic index predictions were made 15.3 and 4.3 hours before the CME shock arrival at L1, and 33.9 and 10.3 hours ahead of peak storm time; a large improvement over current L1-based nowcasting capabilities. Analysis reveals that simple drag-based models, when observationally constrained by upstream in situ observations, improved arrival time estimates, comparable to more complex models, though arrival time errors of several hours persist. Our results show that good predictions of CME magnetic structure and geomagnetic indices with actionable lead-times can be made with far upstream spacecraft, even with longitudinal separations up to 10° from the Sun-Earth line, over heliocentric distance ranges where radial evolution effects dominate over longitudinal effects. Limitations include different expansion behaviors for individual CMEs and regions within. Future missions providing continuous data, including solar wind plasma parameters alongside magnetic field measurements, could account for preexisting disturbed conditions and improve geomagnetic prediction accuracy. Our findings demonstrate the substantial value of real-time upstream solar wind measurements for enhancing geomagnetic forecasting accuracy at Earth and provide critical validation for future dedicated upstream space weather missions.
