Monitoring the Solar Wind Before It Reaches L1

Abstract Space weather predictions of the solar wind impacting Earth are usually first based on remote‐sensing observations of the solar disc and corona, and eventually validated and/or refined with in situ measurements taken at the Sun–Earth Lagrange L1 point, where real‐time monitoring probes are located. However, this pipeline provides, on average, only a few tens of minutes of lead time, which decreases to min or less for large solar wind speeds of km and above. The G5 geomagnetic storm of 2024 May provided an opportunity to test predictions generated employing real‐time data from the STEREO‐A spacecraft, placed west of Earth and 0.04 au closer to the Sun than L1 at the time of the event, as shown recently by Weiler et al. (2025, https://doi.org/10.1029/2024sw004260 ). In this Commentary, we contextualize these results to reflect upon the advantages of measuring the solar wind in situ upstream of L1, leading to improvements in both fundamental research of interplanetary physics and space weather predictions of the near‐Earth environment.