SM042-0005
Quantitative Model of Subauroral Polarization Stream Based on Global MHD Simulations
Abstract:
magnetosphere, the low-latitude cutoff of electron precipitation, and the resulting low conductance in the SAPS flow channel. SAPS flows are thought to increase the recombination rate, which further reduces the conductance in the SAPS channel and thus provides a positive feedback that can increase the SAPS strength. While the qualitative SAPS model seems to be well established, it is important to quantify the role of these parameters in SAPS formation.
In this study, we use observations from DMSP and Incoherent Scatter Radar (ISR), as well as the physics-based OpenGGCM-RCM-CTIM model that self consistently simulates the coupled magnetosphere-ionosphere-thermosphere (MIT) system. After comparing simulation result with observation, we perform numerical experiments to investigate the effect of the ionosphere parameters on the SAPS. R2 FAC, recombination rate, electron precipitation, and conductance boundary are modified, and their effects on SAPS is investigated. Initial results show that without recombination SAPS would be significant weaker. Also, turning off the R2 currents in the model basically eliminates the SAPS, showing that the R2 currents are the primary SAPS driver.