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Plasma wave interactions with energetic ions near the magnetic equator

Donald A. Gurnett
- 01 Jun 1976 - 
- Vol. 81, Iss: 16, pp 2765-2770
TLDR
In this article, it is suggested that these waves are interacting with energetic protons, alpha particles, and other heavy ions trapped near the magnetic equator, and the possible role these waves play in controlling the distribution of the energetic ions is considered.
Abstract
An intense band of electromagnetic noise is frequently observed near the magnetic equatorial plane at radial distance from about 2 to 5 Re. Recent wideband wave-form measurements with the IMP-6 and Hawkeye-1 satellites have shown that the equatorial noise consists of a complex superposition of many harmonically spaced lines. Several distinctly different frequency spacings are often evident in the same spectrum. The frequency spacing typically ranges from a few Hz to a few tens of Hz. It is suggested that these waves are interacting with energetic protons, alpha particles, and other heavy ions trapped near the magnetic equator. The possible role these waves play in controlling the distribution of the energetic ions is considered.

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Journal ArticleDOI

The terrestrial ring current: Origin, formation, and decay

TL;DR: The ring current is formed by the injection of ions originating in the solar wind and the terrestrial ionosphere and undergo an azimuthal drift as mentioned in this paper, resulting in a rapid intensification of the ring current and an O 1 dominance around storm maximum.
Journal ArticleDOI

Electron acceleration in the Van Allen radiation belts by fast magnetosonic waves

TL;DR: In this article, fast magnetosonic waves, detected by Cluster 3, can accelerate electrons between ∼10 keV and a few MeV inside the outer radiation belt, which is required to explain electron flux increases in the outer Van Allen radiation belt during magnetic storms.
Journal ArticleDOI

Slot region electron loss timescales due to plasmaspheric hiss and lightning‐generated whistlers

TL;DR: In this article, the relative importance of plasmaspheric hiss and lightning-generated whistlers in the slot region and beyond was assessed using the pitch angle and energy diffusion of Ions and Electrons (PADIE) code with global models of the spectral distributions of the wave power.
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A systematic study of ULF Waves Above FH+ from GEOS 1 and 2 Measurements and Their Relationships with proton ring distributions

TL;DR: In this article, a detailed analysis of the ULF noise observed on the GEOS magnetic antennas in the frequency range ∼0.2'12 Hz has revealed the properties of structured emissions occurring just above the proton gyrofrequency whose existence was reported by Russell et al. (1970) and Gurnett (1976).
References
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Book

The theory of plasma waves

T. H. Stix
Journal ArticleDOI

Satellite observations of energetic heavy ions during a geomagnetic storm.

TL;DR: For example, during the geomagnetic storm of December 17, 1971, large fluxes of energetic heavy ions (M / q ≈ 16) were observed in the inner magnetosphere.
Journal ArticleDOI

On the extraterrestrial ring current during geomagnetic storms

TL;DR: In this article, Ogo 3 measurements of proton and electron differential energy spectrums were used to detect charged particles of extraterrestrial ring current during geomagnetic storms, with Ogo
Journal ArticleDOI

VLF electric field observations in the magnetosphere

TL;DR: Magnetospheric VLF electric field emissions above electron cyclotron frequency from OGO 5 observation at magnetic equator were reported in this paper, showing that the magnetic field is magnetic at the equator.
Journal ArticleDOI

OGO 3 observations of ELF noise in the magnetosphere: 2. The nature of the equatorial noise

TL;DR: In this article, an examination of the noise present between 1 and 1000 Hz at the magnetic equator with the OGO 3 search coil magnetometer has revealed a previously unobserved class of signals existing only in the outer plasmasphere.
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