Electron‐Scale Energy Transfer Due To Lower Hybrid Waves During Asymmetric Reconnection

Abstract We use Magnetospheric Multiscale mission data to investigate electron‐scale energy transfer due to lower hybrid drift waves during magnetopause reconnection. We analyze waves observed in an electron‐scale plasma mixing layer at the edge of the magnetospheric outflow. Using high‐resolution electron moments, we obtain an electron current density with a Nyquist frequency of , sufficient to resolve most of the lower hybrid drift wave power observed in the event. We then employ wavelet analysis to evaluate , which accounts for the phase differences between the fluctuating quantities. The analysis shows that the energy exchange is localized within the plasma mixing layer, and it is highly fluctuating, with energy bouncing between waves and electrons throughout the analyzed time and frequency range. However, the cumulative sum over time indicates a net energy transfer from the waves to electrons. We observe an anomalous electron flow toward the magnetosphere, consistent with diffusion and electron mixing. These results indicate that waves and electrons interact dynamically to dissipate the excess internal energy accumulated by sharp density gradients. We conclude that the electron temperature profile within the plasma mixing layer is produced by a combination of electron diffusion across the layer, as well as heating by large‐scale parallel potential and lower hybrid drift waves.