Radio Emission from Atmosphere-Skimming Cosmic Ray Showers in High-Altitude Balloon-Borne Experiments

TL;DR

This paper characterizes the radio emission properties of atmosphere-skimming cosmic ray showers in high-altitude balloon experiments, highlighting unique asymmetries caused by atmospheric and magnetic effects.

Contribution

It provides a detailed simulation-based analysis of radio signals from atmosphere-skimming showers, emphasizing their distinctive asymmetries and implications for balloon-borne detection.

Findings

Refractive asymmetry in electric field distribution due to atmospheric density gradient.

Coherence asymmetry in signal intensity caused by Earth's magnetic field.

Significant differences in radio emission compared to downward-going showers.

Abstract

Atmosphere-skimming air showers are initiated by cosmic rays with incoming directions that allow the cascade to develop entirely within the atmosphere, without reaching the ground. Radio pulses induced by this type of showers have already been observed in balloon-borne experiments such as ANITA, but a detailed characterisation of their properties is lacking. The extreme range of densities in which these cascades can develop gives rise to a wide range of shower profiles, with radio emission characteristics that can differ significantly from those of regular downward-going showers. In this work, we have used the ZHAireS-RASPASS program to characterise the expected radio emission from atmosphere-skimming air showers and its properties. We have studied the interplay between the magnetic field and atmospheric density profile in the expected radio signal, focusing on its detection aboard balloon-borne experiments. The almost horizontal geometry of the events gives rise to a significant \textit{refractive} asymmetry in the spatial distribution of the electric field, due to the propagation of the radio signals across a gradient of index of refraction. In addition, a unique \textit{coherence} asymmetry appears in the intensity of the signals, as a consequence of the cumulative effect of the Earth's magnetic field over the very long distances that these particle cascades traverse. The implications of the peculiar characteristics of the emission are discussed regarding their impact both on the interpretation of collected data and in the exposure of balloon-borne experiments