Ulysses Radio and Plasma Wave Observations at High Southern Heliographic Latitudes

dc.contributor.authorStone, R G
dc.contributor.authorMacdowall, R J
dc.contributor.authorFainberg, J
dc.contributor.authorKaiser, M L
dc.contributor.authorDesch, M D
dc.contributor.authorGoldstein, Melvyn
dc.contributor.authorHoang, S
dc.contributor.authorBougeret, J L
dc.contributor.authorHarvey, C C
dc.contributor.authorManning, R
dc.contributor.authorSteinberg, J L
dc.contributor.authorKellogg, P J
dc.contributor.authorLin, N
dc.contributor.authorGoetz, K
dc.contributor.authorOsherovich, V A
dc.contributor.authorReiner, M J
dc.contributor.authorCanu, P
dc.contributor.authorCornilleau-Wehrlin, N
dc.contributor.authorLengyel-Frey, D
dc.contributor.authorThejappa, G
dc.date.accessioned2023-11-07T19:12:10Z
dc.date.available2023-11-07T19:12:10Z
dc.date.issued1995-05-19
dc.description.abstractUlysses spacecraft radio and plasma wave observations indicate that some variations in the intensity and occurrence rate of electric and magnetic wave events are functions of heliographic latitude, distance from the sun, and phase of the solar cycle. At high heliographic latitudes, solar type III radio emissions did not descend to the local plasma frequency, in contrast to the emission frequencies of some bursts observed in the ecliptic. Short-duration bursts of electrostatic and electromagnetic waves were often found in association with depressions in magnetic field amplitude, known as magnetic holes. Extensive wave activity observed in magnetic clouds may exist because of unusually large electron-ion temperature ratios. The lower number of intense in situ wave events at high latitudes was likely due to the decreased variability of the high- latitude solar wind.en
dc.description.sponsorshipThe French contributions to this experiment have been funded by the Centre National des Etudes Spatiales and the Centre National de la Recherche Scientifique. We thank A. Balogh and J. L. Phillips for permission to publish the solar wind and magnetic field data presented in Figs. 3, 4, and 5.en
dc.description.urihttps://www.science.org/doi/10.1126/science.268.5213.1026en
dc.format.extent4 pagesen
dc.genrejournal articlesen
dc.identifierdoi:10.13016/m2gp4c-nesz
dc.identifier.citationR. G. Stone et al. ,Ulysses Radio and Plasma Wave Observations at High Southern Heliographic Latitudes. Science 268, 1026-1029 (1995). DOI:10.1126/science.268.5213.1026en
dc.identifier.urihttps://doi.org/10.1126/science.268.5213.1026
dc.identifier.urihttp://hdl.handle.net/11603/30568
dc.language.isoenen
dc.publisherAmerican Association for the Advancement of Scienceen
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Goddard Planetary Heliophysics Institute (GPHI)
dc.rightsPublic Domain Mark 1.0*
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.en
dc.rights.urihttp://creativecommons.org/publicdomain/mark/1.0/*
dc.titleUlysses Radio and Plasma Wave Observations at High Southern Heliographic Latitudesen
dc.typeTexten
dcterms.creatorhttps://orcid.org/0000-0002-5317-988Xen

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