Dayside and nightside magnetic field responses at 780 km altitude to dayside reconnection
K. Snekvik, N. {\O}stgaard, P. Tenfjord, J. P. Reistad, K. M. Laundal,, S. E. Milan, and S. E. Haaland

TL;DR
This study investigates how the Earth's ionospheric magnetic field responds to dayside magnetic reconnection, revealing both immediate and delayed responses and proposing a new explanation involving MHD wave propagation.
Contribution
It introduces a new explanation for the immediate ionospheric response to reconnection, based on MHD wave propagation in the magnetosphere, expanding the Cowley-Lockwood paradigm.
Findings
Immediate magnetic field response near noon and midnight.
Reconfiguration time of 10-20 minutes for convection patterns.
A new model explaining immediate response via MHD wave propagation.
Abstract
During southward interplanetary magnetic field, dayside reconnection will drive the Dungey cycle in the magnetosphere, which is manifested as a two-cell convection pattern in the ionosphere. We address the response of the ionospheric convection to changes in the dayside reconnection rate by examining magnetic field perturbations at 780 km altitude. The Active Magnetosphere and Planetary Electrodynamics Response Experiment data products derived from the Iridium constellation provide global maps of the magnetic field perturbations. Cluster data just upstream of the Earth's bow shock have been used to estimate the dayside reconnection rate. By using a statistical model where the magnetic field can respond on several time scales, we confirm previous reports of an almost immediate response both near noon and near midnight combined with a 10-20 min reconfiguration time of the two-cell…
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Taxonomy
TopicsIonosphere and magnetosphere dynamics · Dark Matter and Cosmic Phenomena · Astro and Planetary Science
