Above 10\(^{15}\) eV, the CR flux drops below a few tens of particles per m\(^2\)-year. It is no longer possible to detect the incident particles above the atmosphere before they interact. Direct experiments (characterized by a small geometrical factor \(A\cdot \varDelta \varOmega \) [cm\(^2\) sr]) must be replaced by ground-based instruments that cover up to several thousands of km\(^2\), the extensive air shower (EAS) arrays. They use a completely different approach to CR measurements, started by pioneering experiments soon after World War II by Auger, Kohlhorster and Rossi. The EAS arrays are in most cases large area and long duration experiments studying, as accurately as possible, the nature, flux, mass, direction of primary CRs up to the highest energies. Air showers are initiated by primary CRs, through the interaction with a nucleus in the atmosphere. In addition to the hadronic component the decays of short-lived hadrons lead to a shower of particles: photons, electrons, and positrons constitute the electromagnetic (EM) component; muons and neutrinos constitute the penetrating component. All these particles travel at the speed of light in the atmosphere approximately along the direction of the primary CR. High energy primary \(\gamma \)-rays induce an almost pure EM cascade. In Sect. 4.3 we present a simple model for the EM cascade initiated by a \(\gamma \)-ray, which can be mathematically treated using differential transport equations of \(e^\pm \) and \(\gamma \) in the atmosphere. Some simple features, as derived from approximate solutions of the cascade equations, are presented. The cascades initiated by primary CR protons or nuclei have additional features. They are also characterized by large event-to-event fluctuations. Their description is today achieved using full Monte Carlo simulations, which follow the details of the development of the EM and muonic components. It is interesting, however, to obtain (Sect. 4.4) a first-order estimate of the quantities, which can be measured by experiments both for the muonic and the EM components. In the first sections of the chapter, we enumerate the main showers features (denoted as SF1, SF2,..., SF12)) which characterize EM and muonic component of the cascade initiated by \(\gamma \)-rays, protons, and heavier nuclei. These characteristics are confirmed by detailed Monte Carlo simulations of air showers in the atmosphere (Sect. 4.5), which are used by the experiments to interpret their observations. EAS arrays are installed on ground and are sometimes referred to as indirect detection experiments. Modern shower arrays employ complementary techniques (Sect. 4.6) such as scintillators, air Cherenkov detectors, etc. to measure simultaneously as many shower parameters as possible, in order to reduce the model dependence in the energy and mass number \(A\) determination. The features of the EM and muonic cascades will be used in Sects. 4.8, 4.9 and 4.10 to illustrate how indirect experiments can derive the CR flux and properties in the energy region around the knee of CRs.
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