HIGHLIGHTS
SUMMARY
2011; Artemyev et_al, 2017; Grigorenko et_al, 2019; Sitnov et_al, 2019; Kronberg et_al, 2021). The Moon is then also very well situated to study atmospheric escape from the Earth into space (Lammer et_al, 2008; Harnett et_al, 2013; Wei et_al, 2020; André et_al, 2021; Dandouras, 2021; Wang et_al, 2021), in the form of heavy ions upwelling from the terrestrial ionosphere and transported and lost into the deep magnetotail. Far magnetotail studies performed by the Geotail spacecraft supplied key information on the dynamics of ion beams streaming downtail (Christon et_al, 1994; Seki et_al, 1998; Christon et_al, 2020 . . .
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