“…The terrestrial magnetosheath is often populated by high-speed plasma jets (also called plasmoids or plasma irregularities) streaming towards the frontside magnetopause (e.g., Dmitriev andSuvorova, 2012, 2015;Karlsson et al, 2012;Gunell et al, 2014) and impact it several times per hour (Plaschke et al, 2016). These finite-size plasma structures have an excess of antisunward dynamic pressure with respect to the ambient magnetosheath (e.g., Hietala et al, 2012;Savin 20 et al, 2012;Archer and Horbury, 2013;Plaschke et al, 2013Plaschke et al, , 2017Karlsson et al, 2018) and their interaction with the magnetopause can trigger local and global magnetospheric and geophysical effects (e.g., Plaschke et al, 2009;Hietala et al, 2012Hietala et al, , 2018.…”