Driven by the intense solar wind in the inner heliosphere, Mercury's magnetosphere is known to be small and dynamic. Mercury's weak dipole magnetic field of 190 nT-𝐴𝐴 𝐴𝐴 3 𝑀𝑀 (Anderson et al., 2012), where R M is Mercury's radius, and high solar wind dynamic pressures at Mercury's orbit (∼5-10 times higher at 0.31-0.47 AU than those at 1 AU) result in small spatial dimensions of the magnetosphere with an average subsolar standoff distance of 1.45 R M (Winslow et al., 2013). Consequently, time scales of magnetospheric dynamics driven by the solar wind are considerably short at Mercury (e.g., Siscoe et al., 1975). Our understanding of Mercury's magnetosphere has been greatly advanced thanks to the two previous missions to Mercury, Mariner 10 and MESSENGER, but there remain many open questions as to the plasma sources, energy and mass transport, and particle acceleration processes in Mercury's magnetosphere, and their coupling to the exosphere, surface, and interior of the planet (J.