Magnetopause Dynamics as Inferred from Plasma Observations on Low-Altitude Satellites
2011; American Geophysical Union; Linguagem: Inglês
10.1029/gm090p0407
ISSN2328-8779
Autores Tópico(s)Earthquake Detection and Analysis
ResumoMagnetopause Dynamics as Inferred from Plasma Observations on Low-Altitude Satellites Patrick T. Newell, Patrick T. Newell The Johns Hopkins University Applied Physics Laboratory, Laurel, MarylandSearch for more papers by this authorChing-I. Meng, Ching-I. Meng The Johns Hopkins University Applied Physics Laboratory, Laurel, MarylandSearch for more papers by this author Patrick T. Newell, Patrick T. Newell The Johns Hopkins University Applied Physics Laboratory, Laurel, MarylandSearch for more papers by this authorChing-I. Meng, Ching-I. Meng The Johns Hopkins University Applied Physics Laboratory, Laurel, MarylandSearch for more papers by this author Book Editor(s):P. Song, P. SongSearch for more papers by this authorB.U.Ö. Sonnerup, B.U.Ö. SonnerupSearch for more papers by this authorM.F. Thomsen, M.F. ThomsenSearch for more papers by this author First published: 01 January 1995 https://doi.org/10.1029/GM090p0407Citations: 11Book Series:Geophysical Monograph Series AboutPDFPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShareShare a linkShare onFacebookTwitterLinked InRedditWechat Summary This chapter contains sections titled: Introduction Low-Altitude and Ground-Based Observations as the Preferred Site for Quantitative Agnetopause/Boundary Layer Research Cusp Dispersion: New Evidence About the Velocity Filter Hypothesis and its Application to the Staircase Cusp Citing Literature Physics of the Magnetopause, Volume 90 RelatedInformation
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