- 1GeoSphere Austria, Austrian Space Weather Office, GeoSphere Austria, Graz, Austria (eva.weiler@geosphere.at)
- 2Institute of Physics, University of Graz, Universitätsplatz 5, 8010 Graz, Austria
- 3Space Science Center and Department of Physics and Astronomy, University of New Hampshire, 8 College Rd, Durham, NH 03824, USA
- 4Conrad Observatory, GeoSphere Austria, Hohe Warte 38, Vienna, 1190, Austria
- 5Kanzelhöhe Observatory for Solar and Environmental Research, University of Graz, Kanzelhöhe 19, Treffen am Ossiacher See, 9521, Austria
- 6Community Coordinated Modeling Center, NASA Goddard Space Flight Center, 8800 Greenbelt Rd., Greenbelt, MD 20771, USA
- 7Universities Space Research Association, Washington, DC, USA
We investigate the feasibility and potential forecasting benefits of future sub-L1 missions. Spacecraft positioned sunward of the Sun–Earth L1 point offer a promising opportunity to increase forecast lead times for geoeffective solar-wind structures.
ESA is currently preparing a sub-L1 mission, HENON, scheduled for launch by the end of 2026. HENON is a CubeSat mission on a distant retrograde orbit (DRO) at roughly 0.9 au. A larger follow-on mission, SHIELD, is being studied, consisting of a fleet of spacecraft with an orbit planned at about 0.86 au. Together, these efforts represent the first concrete steps toward operational sub-L1 monitoring. Compared to L1 monitoring, the forecast lead times for CME in situ structures and their geomagnetic impacts are increased by factors of roughly 10 and 14 for HENON and SHIELD, respectively.
In our study, we evaluate key requirements for future sub-L1 missions. To this end, we analyse past observations from spacecraft that have crossed the Sun–Earth line at heliocentric distances of less than 0.95 au, including STEREO-A, Solar Orbiter, and Parker Solar Probe. We assess whether and how these data could be used to reliably reproduce observed geomagnetic storms at Earth. We develop a baseline methodology that continuously time-shifts sub-L1 measurements to Earth and hereafter applies the Temerin and Li solar wind-to-Dst model, enabling a direct comparison between predicted and observed geomagnetic indices.
Exploiting the Sun–Earth line passage of STEREO-A from November 2022 to June 2024, we find that a radial separation to Earth of up to 0.05 au sometimes results in negative lead times, with structures being observed at L1 before STEREO-A. This implies that future sub-L1 monitors must be positioned closer to the Sun than 0.95 au. We also find that stronger geomagnetic events are reproduced best, with 82% of all intense storms being successfully modelled using sub-L1 data. Furthermore, we identify a possible east–west asymmetry in forecast lead time, with higher lead times eastward of the Sun-Earth line than westward. This could, however, be a trajectory effect of STEREO-A and should be systematically investigated by HENON.
Using Solar Orbiter and Parker Solar Probe measurements at even smaller heliocentric distances, we aim to statistically determine an ideal trade-off between increased lead time and forecast accuracy.
How to cite: Weiler, E., Davies, E., Möstl, C., Lugaz, N., Bailey, R., Veronig, A., and Reiss, M.: Potential benefits of future sub-L1 missions (HENON, SHIELD) for space weather forecasting, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-9450, https://doi.org/10.5194/egusphere-egu26-9450, 2026.