Observations of relativistic energetic electron fluxes in the outer radiation belt can show dropouts, i.e., sudden electron flux depletions during the main phase of a geomagnetic storm. Many recent studies show that these dropouts typically involve a true loss of particles i.e. non‐adiabatic losses in nature. Precipitation into the atmosphere of relativistic electrons driven into the bounce loss cone, through wave particle interactions, is envisaged as one of the primary loss mechanisms. Such precipitation can be studied using ground based observations such as VLF narrow‐band radio waves, due to the deposition of energy into the lower ionospheric D‐region, thereby modifying the sub‐ionospheric waveguide. The present study focuses on the dropout event observed during the St. Patrick’s Day storm of March 2015. Perturbations lasting several hours were observed in the received VLF amplitude and phase of the NAA transmitter signal measured at Seattle and Edmonton, and the NML transmitter signal received at St. John’s and Edmonton. All these L≈3‐4.5 paths were located on the night‐side of the Earth during dropout phase of the storm. Observations of relativistic electron characteristics from Van Allen Probes, and ionospheric perturbation characterization from VLF radio waves, are used to calculate that during the time interval of the dropout event <0.5% of the relativistic fluxes involved in the dropout event were lost to the atmosphere. This leads to the conclusion that relativistic electron precipitation was not the major contributor to the observed dropout event at L≈4 that occurred during the St. Patrick's Day storm of March 2015.
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