EGU26-6038, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-6038
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 14:10–14:20 (CEST)
 
Room -2.20
Initial TRACERS Observations of Auroral Electron Precipitation: Case Studies of Diffuse and Discrete Aurora
Sarah Henderson1, Jasper Halekas1, Robert Strangeway2, Scott Bounds1, Ivar Christopher1, Aidan Moore1, Suranga Ruhunsuri3, and David Miles1
Sarah Henderson et al.
  • 1University of Iowa, Physics and Astronomy, Iowa City, IA, United States of America
  • 2University of California Los Angeles, Los Angeles, CA, United States of America
  • 3University of Colorado Boulder, Laboratory for Atmospheric and Space Physics, Boulder, CO, United States of America

The Tandem Reconnection and Cusp Electrodynamics Reconnaissance Satellites (TRACERS) is a recently launched NASA mission focused on investigating how temporal or spatial variations in magnetic reconnection drive cusp dynamics by employing multipoint, high-cadence measurements from two identical spacecraft. TRACERS successfully launched into a Sun-synchronous 590 km orbit around Earth on July 23, 2025. The two spacecraft comprising TRACERS are equipped with identical instrument payloads capable of measuring ions, electrons, and electromagnetic fields within low-Earth orbit. The primary goal of the TRACERS mission is to disentangle temporal and spatial variation of magnetic reconnection and associated processes by employing multipoint measurements within the cusp from two identical spacecraft (TRACERS-1 and -2), which are separated by 10 to 120 seconds. In addition to its primary science goals of examining cusp dynamics, TRACERS is also capable of measuring auroral precipitation and processes with high spatial and temporal resolution. We present initial auroral electron observations from one of the TRACERS spacecraft on October 7, 2025. We observe both discrete and diffuse electron precipitation in two orbits in the northern hemisphere. TRACERS-2 observes numerous inverted-V structures indicative of discrete aurora within the auroral oval and polar cap, as well as within the northern cusp. Hours later, TRACERS-2 observes broadband, diffuse electron precipitation spanning tens of eV to tens of keV across the northern polar cap, indicative of polar rain. We discuss the upstream solar wind conditions during each observation utilizing Wind data, as well as the characteristic energies, pitch angle distributions, and fluxes of each electron population observed by TRACERS-2 during these two observations.

How to cite: Henderson, S., Halekas, J., Strangeway, R., Bounds, S., Christopher, I., Moore, A., Ruhunsuri, S., and Miles, D.: Initial TRACERS Observations of Auroral Electron Precipitation: Case Studies of Diffuse and Discrete Aurora, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-6038, https://doi.org/10.5194/egusphere-egu26-6038, 2026.