“…During the past few decades, long‐term radon monitoring has been conducted within geological media such as shallow soil, country rock, alluvial deposits, ground water, and hot springs and has revealed the following results: (1) A typical cyclical daily signature in radon temporal variability [ Lehmann et al , ; Martín‐Luis et al , ; Schubert and Schulz , ; Alparone et al , ; Fujiyoshi et al , ; Sundal et al , ; Choubey et al , ]: (2) longer radon signals, of several days [ Steinitz et al , ; Richon et al , ; Barbosa et al , ; Eff‐Darwich et al , ; Inan et al , ; Nikolopoulos et al , ]; and (3) long‐term seasonal patterns [ Perrier et al , ; Ghosh et al , ; Barbosa et al , ; Choubey et al , ; Richon et al , ; Zafrir et al , ; Martin‐Luis et al , ].…”