Absence of the strahl during times of slow wind

dc.contributor.authorGurgiolo, Chris
dc.contributor.authorGoldstein, Melvyn
dc.date.accessioned2024-01-18T02:21:43Z
dc.date.available2024-01-18T02:21:43Z
dc.date.issued2017-01-05
dc.description.abstractAbstract. It is not uncommon during periods when the solar wind speed is less than 425 km s−1 to observe near 1 AU no evidence of a strahl population in either the electron solar wind or within the foreshock. Estimating the fluid flow within each energy step returned from the Plasma Electron And Current Experiment (PEACE) on board Cluster-2 often finds that in slow wind the GSE spherical flow angles in energies above where there is a clear core/halo signature are often close to radial with no evidence of a field-aligned flow. This signifies the lack of a strahl presence in the electron velocity distribution function (eVDF). When there is no obvious strahl signature in the data, the electrons above the core/halo in energy appear to be unstructured and smeared in angle. This can either be interpreted as due to statistical noise in low counting rate situations or the result of intense scattering. Regions where the strahl is seen and not seen are often separated by a very thin boundary layer. These transitions in the spacecraft frame of reference can be quite rapid, generally occurring within one to two spins (4–8 s).
dc.description.sponsorshipThe authors would like to acknowledge the work and role of the Cluster Science Archive (CSA) and thank the EFW and FGM teams for providing the data used in this study. We would also like to acknowledge the PEACE team at MSSL who worked on and are constantly improving the instrument calibration. We thank the ACE SWEPAM instrument team and the ACE Science Center for providing the ACE data. We would like to acknowledge support from NASA Grant NNX15AI88G.
dc.description.urihttps://angeo.copernicus.org/articles/35/71/2017/
dc.format.extent15 pages
dc.genrejournal articles
dc.identifier.citationGurgiolo, C. and Goldstein, M. L.: Absence of the strahl during times of slow wind, Ann. Geophys., 35, 71–85, https://doi.org/10.5194/angeo-35-71-2017, 2017.
dc.identifier.urihttps://doi.org/10.5194/angeo-35-71-2017
dc.identifier.urihttp://hdl.handle.net/11603/31335
dc.language.isoen_US
dc.publisherEGU
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Goddard Planetary Heliophysics Institute (GPHI)
dc.relation.ispartofUMBC Faculty Collection
dc.rightsThis item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author.
dc.rightsAttribution 3.0 Unported (CC BY 3.0 DEED) en
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/
dc.titleAbsence of the strahl during times of slow wind
dc.title.alternativeStrahl characteristics in periods of slow wind
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0002-5317-988X

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