Articles | Volume 44, issue 2
https://doi.org/10.5194/angeo-44-903-2026
https://doi.org/10.5194/angeo-44-903-2026
Regular paper
 | 
04 Sep 2026
Regular paper |  | 04 Sep 2026

Estimating the source altitude of auroral precipitation from dispersed Alfvén waves in the dayside ionosphere

Etienne Gavazzi, Andres Spicher, Björn Gustavsson, Juha Vierinen, James Clemmons, Robert Pfaff, and Douglas Rowland

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Short summary
Auroras are caused by energetic electrons entering the upper atmosphere. For the smallest and most dynamic auroras, scientists think electrons are accelerated by waves (called Alfvén waves) thousands of kilometers above Earth. In this paper, we analyse data from a rocket that flew through auroras, applying existing and new techniques to estimate where the acceleration took place. Our results match theory, and we show how they can be used to study conditions in the near-Earth space environment.
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