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2005 (English)In: Annales Geophysicae, ISSN 0992-7689, E-ISSN 1432-0576, Vol. 23, no 12, p. 3715-3725Article in journal (Refereed) Published
Abstract [en]
Whistler emissions close to the magnetopause on the magnetospheric side are investigated using the four Cluster spacecraft. The waves are found to be generated in thin (electron-scale) sheets moving with the plasma drift velocity. A feature in the electron data coincides with the waves; hot magnetospheric electrons disappear for a few satellite spins. This produces or enhances a temperature anisotropy, which is found to be responsible for the generation of the whistler mode waves. The high energy electrons are thought to be lost through the magnetopause and we suggest that the field lines, on which the waves are generated, are directly connected to a reconnection diffusion region at the magnetopause.
Place, publisher, year, edition, pages
Göttingen: Copernicus gesellschaft, 2005
Keywords
magnetospheric physics, magnetopause, cusp and boundary layers, space plasma physics, magnetic reconnection, waves and instabilities
National Category
Astronomy, Astrophysics and Cosmology Geology Meteorology and Atmospheric Sciences
Identifiers
urn:nbn:se:umu:diva-4596 (URN)10.5194/angeo-23-3715-2005 (DOI)000235008400013 ()2-s2.0-30844473789 (Scopus ID)
2005-05-132005-05-132025-02-01Bibliographically approved