W. S. Kurth, J. B. Faden, J. H. Waite, A. H. Sulaiman, S. S. Elliott, G. B. Hospodarsky, J. E. P. Connerney, J. A. Kammer, T. Greathouse, P. Valek, F. Allegrini, F. Bagenal, T. Stallard, L. Moore, D. A. Coffin, O. Agiwal, P. Withers, S. J. Bolton
{"title":"Electron Densities in Jupiter's Upper Ionosphere Inferred From Juno Plasma Wave Observations","authors":"W. S. Kurth, J. B. Faden, J. H. Waite, A. H. Sulaiman, S. S. Elliott, G. B. Hospodarsky, J. E. P. Connerney, J. A. Kammer, T. Greathouse, P. Valek, F. Allegrini, F. Bagenal, T. Stallard, L. Moore, D. A. Coffin, O. Agiwal, P. Withers, S. J. Bolton","doi":"10.1029/2024JE008845","DOIUrl":null,"url":null,"abstract":"<p>Juno's highly eccentric polar orbit takes it to perijove distances of <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation> ${\\sim} $</annotation>\n </semantics></math>1.06 <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>R</mi>\n <mi>J</mi>\n </msub>\n </mrow>\n <annotation> ${\\mathrm{R}}_{J}$</annotation>\n </semantics></math> on each orbit. For the first perijove, this occurred just north of the jovigraphic equator, but has precessed north by about a degree per orbit over the mission. Minimum altitudes vary from <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation> ${\\sim} $</annotation>\n </semantics></math>3,200–8,000 km through the mission. The Waves instrument observes a number of plasma wave modes in and near the non-auroral ionosphere that provide information on the local electron number density, including electron plasma oscillations that occur at the electron plasma frequency <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>f</mi>\n <mrow>\n <mi>p</mi>\n <mi>e</mi>\n </mrow>\n </msub>\n </mrow>\n <annotation> ${f}_{pe}$</annotation>\n </semantics></math> and whistler-mode hiss which has an upper frequency limit of <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>f</mi>\n <mrow>\n <mi>p</mi>\n <mi>e</mi>\n </mrow>\n </msub>\n </mrow>\n <annotation> ${f}_{pe}$</annotation>\n </semantics></math> in Jupiter's strongly magnetized inner magnetosphere. The electron plasma frequency provides the electron number density. We present electron densities in the topside ionosphere, similar to Earth's F2 layer, from the <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation> ${\\sim} $</annotation>\n </semantics></math>59 perijoves analyzed to date. Peak densities range from <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation> ${\\sim} $</annotation>\n </semantics></math>100 to 80,000 <span></span><math>\n <semantics>\n <mrow>\n <msup>\n <mtext>cm</mtext>\n <mrow>\n <mo>−</mo>\n <mn>3</mn>\n </mrow>\n </msup>\n </mrow>\n <annotation> ${\\text{cm}}^{-3}$</annotation>\n </semantics></math> at latitudes up to <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n <mn>40</mn>\n <mo>°</mo>\n </mrow>\n <annotation> ${\\sim} 40{}^{\\circ}$</annotation>\n </semantics></math>. The density profiles can be highly variable from one perijove to the next. And, there can be deviations from simple smooth variations with altitude within individual ionospheric passes. Spatial variations may be responsible for some of the variability, perhaps related to Jupiter's complex magnetic field. We show the variation in ionospheric density profiles and the distribution of peak densities as a function of latitude and longitude as well as other geometric parameters. In addition to the complex magnetic field, possible factors affecting ionospheric density variations investigated here are ionospheric dynamos analogous to those at Earth and precipitation of energetic particles.</p>","PeriodicalId":16101,"journal":{"name":"Journal of Geophysical Research: Planets","volume":"130 3","pages":""},"PeriodicalIF":3.9000,"publicationDate":"2025-03-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2024JE008845","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Planets","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2024JE008845","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Juno's highly eccentric polar orbit takes it to perijove distances of 1.06 on each orbit. For the first perijove, this occurred just north of the jovigraphic equator, but has precessed north by about a degree per orbit over the mission. Minimum altitudes vary from 3,200–8,000 km through the mission. The Waves instrument observes a number of plasma wave modes in and near the non-auroral ionosphere that provide information on the local electron number density, including electron plasma oscillations that occur at the electron plasma frequency and whistler-mode hiss which has an upper frequency limit of in Jupiter's strongly magnetized inner magnetosphere. The electron plasma frequency provides the electron number density. We present electron densities in the topside ionosphere, similar to Earth's F2 layer, from the 59 perijoves analyzed to date. Peak densities range from 100 to 80,000 at latitudes up to . The density profiles can be highly variable from one perijove to the next. And, there can be deviations from simple smooth variations with altitude within individual ionospheric passes. Spatial variations may be responsible for some of the variability, perhaps related to Jupiter's complex magnetic field. We show the variation in ionospheric density profiles and the distribution of peak densities as a function of latitude and longitude as well as other geometric parameters. In addition to the complex magnetic field, possible factors affecting ionospheric density variations investigated here are ionospheric dynamos analogous to those at Earth and precipitation of energetic particles.
期刊介绍:
The Journal of Geophysical Research Planets is dedicated to the publication of new and original research in the broad field of planetary science. Manuscripts concerning planetary geology, geophysics, geochemistry, atmospheres, and dynamics are appropriate for the journal when they increase knowledge about the processes that affect Solar System objects. Manuscripts concerning other planetary systems, exoplanets or Earth are welcome when presented in a comparative planetology perspective. Studies in the field of astrobiology will be considered when they have immediate consequences for the interpretation of planetary data. JGR: Planets does not publish manuscripts that deal with future missions and instrumentation, nor those that are primarily of an engineering interest. Instrument, calibration or data processing papers may be appropriate for the journal, but only when accompanied by scientific analysis and interpretation that increases understanding of the studied object. A manuscript that describes a new method or technique would be acceptable for JGR: Planets if it contained new and relevant scientific results obtained using the method. Review articles are generally not appropriate for JGR: Planets, but they may be considered if they form an integral part of a special issue.