Revisiting the structure of low-Mach number, low-beta, quasi-perpendicular shocks

A study of the structure of 145 low-Mach number (M <= 3), low-beta (beta <= 1), quasi-perpendicular interplanetary collisionless shock waves observed by the Wind spacecraft has provided strong evidence that these shocks have large-amplitude whistler precursors. The common occurrence and large amplitudes of the precursors raise doubts about the standard assumption that such shocks can be classified as laminar structures. This directly contradicts standard models. In 113 of the 145 shocks (similar to 78%), we observe clear evidence of magnetosonic-whistler precursor fluctuations with frequencies similar to 0.1-7Hz. We find no dependence on the upstream plasma beta, or any other shock parameter, for the presence or absence of precursors. The majority (similar to 66%) of the precursors propagate at <= 45 degrees with respect to the upstream average magnetic field and most (similar to 87%) propagate >= 30 degrees from the shock normal vector. Further, most (similar to 79%) of the waves propagate at least 20 degrees from the coplanarity plane. The peak-to-peak wave amplitudes (delta Bpk-pk) are large with a range of maximum values for the 113 precursors of similar to 0.2-13 nT with an average of similar to 3 nT. When we normalize the wave amplitudes to the upstream averaged magnetic field and the shock ramp amplitude, we find average values of similar to 50% and similar to 80%, respectively. Plain Language Summary We present new results that suggest that the magnetic structure of collisionless shock waves is not a smooth, step-like transition but rather riddled with large-amplitude waves as large or larger than the shock itself. These results have implications for the dynamics of weak shocks from propagation and evolution to particle acceleration and heating.