“…M‐components are characterized by a transient increase in the current and the luminosity of lightning channels carrying a continuing current that follows some return strokes (Fisher et al, 1993; Malan & Collens, 1937; Thottappillil et al, 1995, Wang et al, 1999). Experimental data on M‐components are available from natural lightning (e.g., Campos et al, 2007; Shao et al, 1995; Stolzenburg et al, 2015; Vayanganie et al, 2014), instrumented towers (e.g., Azadifar et al, 2016; Flache et al, 2008; He, Azadifar, Li, et al, 2018; He, Azadifar, Rachidi, et al, 2018; Miki et al, 2005, 2006; Paul & Heidler , 2018; Pichler & Diendorfer, 2010; Visacro et al, 2013; Zhou et al, 2015), and triggered lightning (e.g., Qie et al, 2011; Rakov et al, 1995, 2001; Tran et al, 2013; Zhang et al, 2017). Only in the latter two cases (instrumented towers and triggered lightning) were the channel‐base currents measured simultaneously with the M‐component fields.…”