Modeling extreme “Carrington‐type” space weather events using three‐dimensional global MHD simulations

There is a growing concern over possible severe societal consequences related to adverse space weather impacts on man‐made technological infrastructure. In the last two decades, significant progress has been made toward the first‐principles modeling of space weather events, and three‐dimensional (3‐D) global magnetohydrodynamics (MHD) models have been at the forefront of this transition, thereby playing a critical role in advancing our understanding of space weather. However, the modeling of extreme space weather events is still a major challenge even for the modern global MHD models. In this study, we introduce a specially adapted University of Michigan 3‐D global MHD model for simulating extreme space weather events with a Dstfootprint comparable to the Carrington superstorm of September 1859 based on the estimate by Tsurutani et. al. (2003). Results are presented for a simulation run with “very extreme” constructed/idealized solar wind boundary conditions driving the magnetosphere. In particular, we describe the reaction of the magnetosphere‐ionosphere system and the associated induced geoelectric field on the ground to such extreme driving conditions. The model setup is further tested using input data for an observed space weather event of Halloween storm October 2003 to verify the MHD model consistence and to draw additional guidance for future work. This extreme space weather MHD model setup is designed specifically for practical application to the modeling of extreme geomagnetically induced electric fields, which can drive large currents in ground‐based conductor systems such as power transmission grids. Therefore, our ultimate goal is to explore the level of geoelectric fields that can be induced from an assumed storm of the reported magnitude, i.e., Dst∼=−1600 nT. Global MHD simulation of extreme Carrington‐type space weather eventDiscuss reaction of magnetosphere‐ionosphere system to extreme drivingProvide results off extreme geomagnetically induced electric fields