Suprathermal electron flux peaks at stream interfaces: Signature of solar wind dynamics or tracer for open magnetic flux transport on the Sun?

The high variability of the intensity of suprathermal electron flux in the solar wind is usually ascribed to the high variability of sources on the Sun. Here we demonstrate that a substantial amount of the variability arises from peaks in stream interaction regions, where fast wind runs into slow wi...

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Published inJournal of Geophysical Research: Space Physics Vol. 115; no. A11
Main Authors Crooker, N. U., Appleton, E. M., Schwadron, N. A., Owens, M. J.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.11.2010
American Geophysical Union
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Abstract The high variability of the intensity of suprathermal electron flux in the solar wind is usually ascribed to the high variability of sources on the Sun. Here we demonstrate that a substantial amount of the variability arises from peaks in stream interaction regions, where fast wind runs into slow wind and creates a pressure ridge at the interface. Superposed epoch analysis centered on stream interfaces in 26 interaction regions previously identified in Wind data reveal a twofold increase in 250 eV flux (integrated over pitch angle). Whether the peaks result from the compression there or are solar signatures of the coronal hole boundary, to which interfaces may map, is an open question. Suggestive of the latter, some cases show a displacement between the electron and magnetic field peaks at the interface. Since solar information is transmitted to 1 AU much more quickly by suprathermal electrons compared to convected plasma signatures, the displacement may imply a shift in the coronal hole boundary through transport of open magnetic flux via interchange reconnection. If so, however, the fact that displacements occur in both directions and that the electron and field peaks in the superposed epoch analysis are nearly coincident indicate that any systematic transport expected from differential solar rotation is overwhelmed by a random pattern, possibly owing to transport across a ragged coronal hole boundary.
AbstractList The high variability of the intensity of suprathermal electron flux in the solar wind is usually ascribed to the high variability of sources on the Sun. Here we demonstrate that a substantial amount of the variability arises from peaks in stream interaction regions, where fast wind runs into slow wind and creates a pressure ridge at the interface. Superposed epoch analysis centered on stream interfaces in 26 interaction regions previously identified in Wind data reveal a twofold increase in 250 eV flux (integrated over pitch angle). Whether the peaks result from the compression there or are solar signatures of the coronal hole boundary, to which interfaces may map, is an open question. Suggestive of the latter, some cases show a displacement between the electron and magnetic field peaks at the interface. Since solar information is transmitted to 1 AU much more quickly by suprathermal electrons compared to convected plasma signatures, the displacement may imply a shift in the coronal hole boundary through transport of open magnetic flux via interchange reconnection. If so, however, the fact that displacements occur in both directions and that the electron and field peaks in the superposed epoch analysis are nearly coincident indicate that any systematic transport expected from differential solar rotation is overwhelmed by a random pattern, possibly owing to transport across a ragged coronal hole boundary.
Author Appleton, E. M.
Owens, M. J.
Crooker, N. U.
Schwadron, N. A.
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  organization: Space Environment Physics Group, Department of Meteorology, University of Reading, Reading, UK
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Issue A11
Keywords Magnetic flux
Plasma
magnetic field
Pitch angle
variability
electrons
Superposed epoch analysis
dynamics
displacements
direction
Electron flux
interfaces
maps
tracers
streams
cartography
pressure
transport
Sun
solar wind
intensity
Solar rotation
Coronal hole
compression
Suprathermal particle
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Snippet The high variability of the intensity of suprathermal electron flux in the solar wind is usually ascribed to the high variability of sources on the Sun. Here...
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SubjectTerms Astronomy
Astrophysics
coronal hole boundary
Earth sciences
Earth, ocean, space
Exact sciences and technology
Fluctuations
interchange reconnection
Magnetic fields
Planetology
Space
stream interaction region
Sun
Title Suprathermal electron flux peaks at stream interfaces: Signature of solar wind dynamics or tracer for open magnetic flux transport on the Sun?
URI https://api.istex.fr/ark:/67375/WNG-7VCCHC2F-9/fulltext.pdf
https://onlinelibrary.wiley.com/doi/abs/10.1029%2F2010JA015496
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Volume 115
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