“…Interplanetary (IP) shocks are solar wind perturbations that directly trigger geomagnetic activity in the magnetosphere-ionosphere-thermosphere (MIT) system. IP shocks rapidly trigger magnetic sudden impulses in geosynchronous orbit (Wang et al, 2009), magnetotail (Huttunen et al, 2005), and on the ground (Smith et al, 1986;Echer et al, 2005;Smith et al, 2020;Hajra et al, 2020); enhance field-aligned currents (Belakhovsky et al, 2017;Kasran et al, 2019), trigger auroral substorms (Kokubun et al, 1977;Zhou and Tsurutani, 2001;Yue et al, 2010), cause dayside auroras (Zhou and Tsurutani, 1999;Tsurutani et al, 2001;Zhou et al, 2003), affect radiation belts (Schiller et al, 2016;Bhaskar et al, 2021), excite magnetospheric ultra-low frequency (ULF) waves (Kangas et al, 2001;Hartinger et al, 2022); cause geomagnetically induced currents (GICs) (Carter et al, 2015;Belakhovsky et al, 2017;Tsurutani and Hajra, 2021), ionospheric total electron content (Chen et al, 2023), and thermospheric neutral mass density enhancements that intensify satellite orbital drag (Shi et al, 2017;Oliveira and Zesta, 2019). Therefore, space weather-related effects can be observed in many regions of the MIT system.…”