Nitrogen fluorescence in air for observing extensive air showers

TL;DR

This paper reviews the nitrogen fluorescence emission in air, crucial for cosmic ray air shower detection, focusing on its dependence on atmospheric conditions and proposing a unified description for improved accuracy.

Contribution

It presents a first analysis towards a common framework for nitrogen fluorescence emission modeling in air shower observations, considering various atmospheric dependencies.

Findings

Dependence of fluorescence yield on pressure and altitude.

Temperature effects on collisional de-excitation rates.

Impact of water vapor on fluorescence emission.

Abstract

Extensive air showers initiate the fluorescence emissions from nitrogen molecules in air. The UV-light is emitted isotropically and can be used for observing the longitudinal development of extensive air showers in the atmosphere over tenth of kilometers. This measurement technique is well-established since it is exploited for many decades by several cosmic ray experiments. However, a fundamental aspect of the air shower analyses is the description of the fluorescence emission in dependence on varying atmospheric conditions. Different fluorescence yields affect directly the energy scaling of air shower reconstruction. In order to explore the various details of the nitrogen fluorescence emission in air, a few experimental groups have been performing dedicated measurements over the last decade. Most of the measurements are now finished. These experimental groups have been discussing their techniques and results in a series of Air Fluorescence Workshops commenced in 2002. At the 8$^{\rm{th}}$ Air Fluorescence Workshop 2011, it was suggested to develop a common way of describing the nitrogen fluorescence for application to air shower observations. Here, first analyses for a common treatment of the major dependences of the emission procedure are presented. Aspects like the contributions at different wavelengths, the dependence on pressure as it is decreasing with increasing altitude in the atmosphere, the temperature dependence, in particular that of the collisional cross sections between molecules involved, and the collisional de-excitation by water vapor are discussed.