Abstract

AbstractKnowledge of the ambient solar wind is important for accurate space weather forecasting. A simple‐but‐effective method of forecasting near‐Earth solar wind speed is “corotation,” wherein solar wind structure is assumed to be fixed in the reference frame rotating with the Sun. Under this approximation, observations at a source spacecraft can be rotated to a target location, such as Earth. Forecast accuracy depends upon the rate of solar wind evolution, longitudinal and latitudinal separation between the source and target, and latitudinal structure in the solar wind itself. The time‐evolution rate and latitudinal structure of the solar wind are both strongly influenced by the solar cycle, though in opposing ways. A latitudinal separation (offset) between source and target spacecraft is typically present, introducing an error to corotation forecasts. In this study, we use observations from the Solar Terrestrial Relations Observatory (STEREO) and near‐Earth spacecraft to quantify the latitudinal error. Aliasing between the solar cycle and STEREO orbits means that individual contributions to the forecast error are difficult to isolate. However, by considering an 18‐month interval near the end of solar minimum, we find that the latitudinal‐offset contribution to corotation forecast error cannot be directly detected for offsets <6°, but is increasingly important as offsets increase. This result can be used to improve solar wind data assimilation, allowing representivity errors in solar wind observations to be correctly specified. Furthermore, as the maximum latitudinal offset between L5 and Earth is ≈5°, corotation forecasts from a future L5 spacecraft should not be greatly affected by latitudinal offset.

Highlights

  • Space weather has the potential to damage electricity grids, cause satellite failures, disrupt communications, and threaten the health of humans in space (Cannon, 2013)

  • High-speed streams emanating from coronal holes can compress into the slower solar wind and form stream interaction regions (SIRs), which become corotating interaction regions (CIRs) if they persist for several solar rotations (Reiss et al, 2016)

  • There is a trend for increasing mean absolute error (MAE) with increasing Δt out to around 7 days

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Summary

Introduction

Space weather has the potential to damage electricity grids, cause satellite failures, disrupt communications, and threaten the health of humans in space (Cannon, 2013). Steady-state structures in the solar wind can be a driver for space weather events in their own right (e.g., Alves et al, 2006). High-speed streams emanating from coronal holes can compress into the slower solar wind and form stream interaction regions (SIRs), which become corotating interaction regions (CIRs) if they persist for several solar rotations (Reiss et al, 2016). These are regions of higher plasma density and magnetic field strength and can cause geomagnetic disturbances

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