The magnetosphere-plasmasphere-ionosphere energy coupling in geospace is one of the key focuses in the space physics and space weather researches. The coupling is primarily represented by the mass, energy and moment in solar wind entering into and convecting in the magnetosphere, transforming between waves and particles in the inner magnetosphere, being released into the ionosphere and upper atmosphere and eventually generating spectacular auroras in the Earth's polar region (e.g., Angelopoulos et al, 2008;Lyon, 2000) and even the equatorial region (He, Wei, & Wan, 2020;He et al, 2021). The inner magnetosphere, as one of the important regions where the mass and energy couple and diffuse, contains the plasmasphere, the ring current and the radiation belts.