How the IMF $\mathit{B}_{y}$ Induces a Local $\mathit{B}_{y}$ Component During Northward IMF $\mathit{B}_{z}$ and Characteristic Timescales
P. Tenfjord, N. {\O}stgaard, S. Haaland, K. Snekvik, K. M. Laundal, J., P. Reistad, R. Strangeway, S. E. Milan, M. Hesse, and A. Ohma

TL;DR
This study uses global MHD simulations and satellite data to analyze how a northward IMF Bz influences the induction of a local By component in Earth's magnetosphere, revealing the timescales and mechanisms involved.
Contribution
It provides a detailed analysis of the induction process of local By during northward IMF Bz conditions, including the timescales and the role of shear flows, which was not previously well characterized.
Findings
Induced By responds within 16 minutes of IMF B y arrival.
Complete reconfiguration of By occurs within 47 minutes.
Asymmetric magnetic energy density influences local By induction.
Abstract
We use the Lyon-Fedder-Mobarry global magnetohydrodynamics model to study the effects of the interplanetary magnetic field (IMF) component on the coupling between the solar wind and magnetosphere-ionosphere system when IMF 0. We describe the evolution of how a magnetospheric component is induced on closed field lines during these conditions. Starting from dayside lobe reconnection, the magnetic tension on newly reconnected field lines redistribute the open flux asymmetrically between the two hemispheres. This results in asymmetric magnetic energy density in the lobes. Shear flows are induced to restore equilibrium, and these flows are what effectively induces a local component. We show the radial dependence of the induced and compare the results to the induced during southward IMF…
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