“…Whistler modes that propagate in the ionosphere and magnetosphere have been excited by ground based transmitters such as SIPLE Antarctica (Helliwell, 1977), the world's high power VLF navigation transmitters (Ma et al., 2017; Meredith et al., 2019; Parrot et al., 2007; Ross et al., 2019; Záhlava et al., 2018; S. Zhao, Zhou, et al., 2019), and the high power HF facilities in Arecibo, Puerto Rico (Pradipta et al., 2007) and HAARP, Alaska (Cohen & Golkowski, 2013; Golkowski et al., 2019), or modulation of energetic electron beams on the Space Shuttle (Carlsten et al., 2019). Three current experimental efforts (Borovsky & Delzanno, 2019) for space‐based VLF wave generation are supported in the United States by (1) the Air Force Research Laboratory with the DSX large dipole antenna operational from June 2019 to transmit VLF waves in space (Scherbarth et al., 2009), (2) the Los Alamos National Laboratory with a VLF precipitation experiment scheduled for April 2021 to launch the Beam Plasma Interactions Experiment (Beam‐PIE) with electron beam generation on a sounding Rocket (Carlsten et al., 2019), and (3) the Naval Research Laboratory with an injection of 1.5 kg of barium to form hypersonic ions that are converted into lower‐hybrid, whistler or magnetosonic waves (Ganguli et al., 2015, 2019). Alternate techniques for whistler mode generation are being studied because these waves are difficult to radiate with conventional antennas where the free space wavelengths (10–1,000 km) are so much longer than a practically realizable vertical monopole antenna, and the radiation efficiency is exceedingly small.…”