Origin of Dawnside Subauroral Polarization Streams During Major Geomagnetic Storms

Solar eruptions cause geomagnetic storms in the near-Earth environment, creating spectacular aurorae visible to the human eye and invisible dynamic changes permeating all of geospace. Just equatorward of the aurora, radars and satellites often observe intense westward plasma flows called subauroral polarization streams (SAPS) in the dusk-to-midnight ionosphere. SAPS occur across a narrow latitudinal range and lead to intense frictional heating of the ionospheric plasma and atmospheric neutral gas. SAPS also generate small-scale plasma waves and density irregularities that interfere with radio communications. As opposed to the commonly observed duskside SAPS, intense eastward subauroral plasma flows in the morning sector were recently discovered to have occurred during a super storm on 20 November 2003. However, the origin of these flows termed dawnside SAPS could not be explained by the same mechanism that causes SAPS on the duskside and has remained a mystery. Through real-event global geospace simulations, here we demonstrate that dawnside SAPS can only occur during major storm conditions. During these times, the magnetospheric plasma convection is so strong as to effectively transport ions to the dawnside, whereas they are typically deflected to the dusk by the energy-dependent drifts. Ring current pressure then builds up on the dawnside and drives field-aligned currents that connect to the subauroral ionosphere, where eastward SAPS are generated. The origin of dawnside SAPS explicated in this study advances our understanding of how the geospace system responds to strongly disturbed solar wind driving conditions that can have severe detrimental impacts on human society and infrastructure.

Automated summary

Solar eruptions cause geomagnetic storms that lead to visible aurorae and invisible dynamic changes in the earth's near-Earth environment. Just equatorward of the aurora, intense westward plasma flows called subauroral polarization streams (SAPS) occur in the dusk-to-midnight ionosphere. These flows generate frictional heating, plasma waves, and density irregularities that interfere with radio communications. Recently, intense eastward subauroral plasma flows in the morning sector called dawnside SAPS were discovered during a super storm. The origin of dawnside SAPS has remained a mystery, but this study shows that they can only occur during major storm conditions. Understanding the origin of dawnside SAPS is important for comprehending the response of the geospace system to strongly disturbed solar wind conditions, which can have severe impacts on human society and infrastructure.