“…Even if long TGEs have been observed in different situations, they have always been associated with thunderstorms. TGEs have been detected at altitudes above 2500 m [ Torii et al , ; Tsuchiya et al , ; Chilingarian et al , , ; Chilingarian and Mkrtchyan , ; Gurevich et al , ], at sea level associated only with winter thunderstorms [ Torii and Sugita , , ], by balloons [ Parks et al , ] and airplanes [ Eack et al , ]. Simulations [ Babich and Loiko , ] have shown that long TGEs are produced inside tropospheric thunderclouds by RREAs of secondary cosmic rays with the source located at 0.5–2 km within the region between the main negative charge and the lower positive charge layer (LPCL), both for those observed at sea level and for those observed at mountain tops [ Chilingarian , ].…”