Control of Magnetopause Flux Rope Topology by Non-local Reconnection

Dayside magnetic reconnection between the interplanetary magnetic field and the Earth’s magnetic field is the primary mechanism enabling mass and energy entry into the magnetosphere. During favorable solar wind conditions, multiple reconnection X-lines can form on the dayside magnetopause, potential...

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Main Authors: Lars Mejnertsen, Jonathan P. Eastwood, Jeremy P. Chittenden
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-11-01
Series:Frontiers in Astronomy and Space Sciences
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fspas.2021.758312/full
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author Lars Mejnertsen
Jonathan P. Eastwood
Jeremy P. Chittenden
author_facet Lars Mejnertsen
Jonathan P. Eastwood
Jeremy P. Chittenden
author_sort Lars Mejnertsen
collection DOAJ
description Dayside magnetic reconnection between the interplanetary magnetic field and the Earth’s magnetic field is the primary mechanism enabling mass and energy entry into the magnetosphere. During favorable solar wind conditions, multiple reconnection X-lines can form on the dayside magnetopause, potentially forming flux ropes. These flux ropes move tailward, but their evolution and fate in the tail is not fully understood. Whilst flux ropes may constitute a class of flux transfer events, the extent to which they add flux to the tail depends on their topology, which can only be measured in situ by satellites providing local observations. Global simulations allow the entire magnetospheric system to be captured at an instant in time, and thus reveal the interconnection between different plasma regions and dynamics on large scales. Using the Gorgon MHD code, we analyze the formation and evolution of flux ropes on the dayside magnetopause during a simulation of a real solar wind event. With a relatively strong solar wind dynamic pressure and southward interplanetary magnetic field, the dayside region becomes very dynamic with evidence of multiple reconnection events. The resulting flux ropes transit around the flank of the magnetosphere before eventually dissipating due to non-local reconnection. This shows that non-local effects may be important in controlling the topology of flux ropes and is a complicating factor in attempts to establish the overall contribution that flux ropes make in the general circulation of magnetic flux through the magnetosphere.
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spelling doaj.art-7a721b75dbbc4d839ac96cbeb4e31c0a2022-12-21T20:28:32ZengFrontiers Media S.A.Frontiers in Astronomy and Space Sciences2296-987X2021-11-01810.3389/fspas.2021.758312758312Control of Magnetopause Flux Rope Topology by Non-local ReconnectionLars Mejnertsen0Jonathan P. Eastwood1Jeremy P. Chittenden2Space and Atmospheric Physics Group, Blackett Laboratory, Imperial College London, London, United KingdomSpace and Atmospheric Physics Group, Blackett Laboratory, Imperial College London, London, United KingdomPlasma Physics Group, Blackett Laboratory, Imperial College London, London, United KingdomDayside magnetic reconnection between the interplanetary magnetic field and the Earth’s magnetic field is the primary mechanism enabling mass and energy entry into the magnetosphere. During favorable solar wind conditions, multiple reconnection X-lines can form on the dayside magnetopause, potentially forming flux ropes. These flux ropes move tailward, but their evolution and fate in the tail is not fully understood. Whilst flux ropes may constitute a class of flux transfer events, the extent to which they add flux to the tail depends on their topology, which can only be measured in situ by satellites providing local observations. Global simulations allow the entire magnetospheric system to be captured at an instant in time, and thus reveal the interconnection between different plasma regions and dynamics on large scales. Using the Gorgon MHD code, we analyze the formation and evolution of flux ropes on the dayside magnetopause during a simulation of a real solar wind event. With a relatively strong solar wind dynamic pressure and southward interplanetary magnetic field, the dayside region becomes very dynamic with evidence of multiple reconnection events. The resulting flux ropes transit around the flank of the magnetosphere before eventually dissipating due to non-local reconnection. This shows that non-local effects may be important in controlling the topology of flux ropes and is a complicating factor in attempts to establish the overall contribution that flux ropes make in the general circulation of magnetic flux through the magnetosphere.https://www.frontiersin.org/articles/10.3389/fspas.2021.758312/fullflux ropereconnectionflux transfer eventsmagnetosphere (magnetospheric configuration and dynamics)global modelling
spellingShingle Lars Mejnertsen
Jonathan P. Eastwood
Jeremy P. Chittenden
Control of Magnetopause Flux Rope Topology by Non-local Reconnection
Frontiers in Astronomy and Space Sciences
flux rope
reconnection
flux transfer events
magnetosphere (magnetospheric configuration and dynamics)
global modelling
title Control of Magnetopause Flux Rope Topology by Non-local Reconnection
title_full Control of Magnetopause Flux Rope Topology by Non-local Reconnection
title_fullStr Control of Magnetopause Flux Rope Topology by Non-local Reconnection
title_full_unstemmed Control of Magnetopause Flux Rope Topology by Non-local Reconnection
title_short Control of Magnetopause Flux Rope Topology by Non-local Reconnection
title_sort control of magnetopause flux rope topology by non local reconnection
topic flux rope
reconnection
flux transfer events
magnetosphere (magnetospheric configuration and dynamics)
global modelling
url https://www.frontiersin.org/articles/10.3389/fspas.2021.758312/full
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AT jeremypchittenden controlofmagnetopausefluxropetopologybynonlocalreconnection