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High latitude ionospheric gradients and their relationships to auroral and magnetospheric boundaries

Por: Chacko, C. C [autor] .Colaborador(es): Mendillo, Michael [autor] .Tipo de material: TextoTextoEditor: Massachusetts: Air Force Geophysics Laboratory, 1977Descripción: 57 páginas: gráficas; 30 cm.Tema(s): IONOSFERA  | AURORAS  | PLASMASFERAClasificación CDD: 551.514/C512
Contenidos:
Chapter 1. Introduction -- Chapter 2. The Baselevel Ionospheric Trough -- Chapter 3. Electron Density enhancements in the F-Region Beneath the magnetospheric cusp -- Chapter 4. The equatorward edge of the diffuse aurora and the poleward wall of the main electron density trough: case study investigations
Resumen: The main electron density trough in the topside ionosphere is investigated using ISIS 2 topside sounder data, DMSP auroral images and ground-based observations. A "base-level" ionospheric trough is characterized with the aid of ISIS 2 electron densities obtained in December 1971 under an optimun set of geophysical conditions, namely midwinter, local midnight and very quiet magnetospheric intervals. The statistical positions of the equatorward and poleward walls of the trough are examined in relation to the plasmapause and various auroral boundaries, respectively.
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Tipo de ítem Colección Signatura Estado Código de barras
Libros Libros Colección Bibliográfica 551.514/C512 (Navegar estantería) Disponible 0002526
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Número de reporte: AFGL-TR-78-0092(I)

Incluye bibliografía

Chapter 1. Introduction -- Chapter 2. The Baselevel Ionospheric Trough -- Chapter 3. Electron Density enhancements in the F-Region Beneath the magnetospheric cusp -- Chapter 4. The equatorward edge of the diffuse aurora and the poleward wall of the main electron density trough: case study investigations

The main electron density trough in the topside ionosphere is investigated using ISIS 2 topside sounder data, DMSP auroral images and ground-based observations. A "base-level" ionospheric trough is characterized with the aid of ISIS 2 electron densities obtained in December 1971 under an optimun set of geophysical conditions, namely midwinter, local midnight and very quiet magnetospheric intervals. The statistical positions of the equatorward and poleward walls of the trough are examined in relation to the plasmapause and various auroral boundaries, respectively.

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