- SM11E-1987: Mercury's Alfvén Wing-Magnetosphere under Sub-Alfvénic Upstream Conditions Driven by ICMEs
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Board 1987‚ Hall EFG (Poster Hall)NOLA CC
Author(s):Generic 'disconnected' Message
Charles Bowers, University of Michigan Ann Arbor (First Author, Presenting Author)
Xianzhe Jia, University of Michigan
Caitriona Jackman, Dublin Institute for Advanced Studies
Lina Hadid, CNRS-LPP
Weijie Sun, University of Michigan
Laura Hayes, Dublin Institute for Advanced Studies (DIAS) Dunsink Observatory
Ryan Dewey, Laboratory for Atmospheric and Space Physics
Brandon Burkholder, Goddard Planetary Heliophysics Institute
Hans Huybrighs, ESA/ESTEC
Matthew James Rutala, Dublin Institute for Advanced Studies
Daragh Hollman, Dublin Institute for Advanced Studies
Sebastian Cervantes, Dublin Institute for Advanced Studies
The Sun continuously emits a stream of plasma, known as the solar wind, which travels through the solar system at hundreds of kilometers per second in all directions.
Normally, the speed of the solar wind far exceeds the speeds at which waves may travel, leading to the formation of shocks on the dayside of planets and other objects in its flow, analogous to shock waves ahead of super-sonic aircraft at Earth. However, in rare cases, the wave speed of the plasma surpasses the speed of the solar wind, which has a direct impact on a planet's magnetic field environment. Here, we explore the implications for this rare regime via observations from the Mercury Surface, Space Environment, Geochemistry, and Ranging (MESSENGER) spacecraft supported by three-dimensional computer simulations. Under these conditions, Mercury does not develop a dayside shock, and its nightside magnetic field differs significantly relative to the typical configuration.These rare solar wind conditions offer brief, but valuable glimpses into the magnetic interactions expected in many exoplanetary systems, where close-in planets are often embedded within a similar stellar wind environment.
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