Several parameters will be collected for each case. First, the nearest upper-air sounding will be examined at the time and altitude most relevant to flash initiation to consider locations of the freezing layer(s), inversion, wind speed and direction, and saturated layers that the aircraft encountered during takeoff or landing. Second, the location of the flash initiation will be searched for events from the National Lightning Detection Network (NLDN), Global Lightning Dataset (GLD360) network, and Geostationary Lightning Mappers (GLMs) on the GOES satellites that will indicate how far the aircraft was located from the nearest flash not initiated by aircraft. Third, the horizontal excursion of the aircraft through these layers will be examined to identify whether the plane navigated from one vertical temperature and dew point distribution to another sounding situation during takeoff or landing.
Preliminary data show that such incidents occurred an average of eight times per year in both the U.S. and globally during the 2014-2024 period. The most annual events in our database were 26 such takeoff and landing cases in 2015, and the fewest was two events in 2021. Events were somewhat more frequent during takeoff than during landing. Cases involved temperatures somewhat above the freezing level, at the freezing level, or below freezing. Such instances imply that more than one form of water particles may be involved as the plane flies through layers around the charging layer vertically, horizontally, or sometimes both. Another five helicopter-induced lightning events are treated separately.
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