Many transient physical processes operate simultaneously and couple nonlinearly in the near-Earth environment across turbulent spatio-temporal scales, producing strong impacts on the cusp, magnetopause and ionosphere that are difficult to fully understand and predict without kinetic simulations. In particular, under quasi-radial interplanetary magnetic field (IMF) conditions the turbulent magnetosheath flow generates large-amplitude, spatially localized dynamic pressure enhancements, known as magnetosheath jets or high-speed jets (Plaschke et al., 2018). These structures, commonly observed by satellites downstream of quasi-parallel bow shocks, carry significant amounts of momentum, energy and magnetic flux. Therefore, their generation mechanism, characteristic lifetimes, physical and geometric properties, and possible impact on the magnetosphere present strong interest to the space physics community.Based on observations in the past two decades, a great amount of statistical knowledge, as well as possible theoretical explanations relating the occurrence of jets to solar wind and foreshock conditions, have been accumulated (Plaschke et al., 2018(Plaschke et al., , 2020. In particular, a theory by Hietala et al. (2012Hietala et al. ( , 2009 suggests that plasma ripples, which inherently develop in the bow shock under quasi-radial IMF and high Mach solar wind conditions, may be responsible for producing local high-speed flows in the magnetosheath by deflecting the incoming solar wind plasma flow in the anti-sunward direction due to the local curvature of a shock front so that the speed of the deflected flow remains close to the upstream solar wind value.