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Open AccessJournal ArticleDOI

Chorus source locations from VLF Poynting flux measurements with the Polar spacecraft

M. J. LeDocq, +2 more
- 01 Nov 1998 - 
- Vol. 25, Iss: 21, pp 4063-4066
TLDR
In this article, a spatial survey of wave normals and Poynting vectors computed from three-component electric and magnetic field measurements is used to show that chorus is generated very close to the magnetic equator.
Abstract
Previous studies have used indirect evidence to argue that whistler-mode chorus emissions are generated near the magnetic equator. In this paper a spatial survey of wave normals and Poynting vectors computed from three-component electric and magnetic field measurements is used to show that chorus is generated very close to the magnetic equator. One surprising result is that there are almost no chorus emissions propagating toward the magnetic equator, such as might be expected from high-latitude magnetospheric reflections. The absence of a reflected component indicates that the chorus is reabsorbed, probably by Landau damping, before returning to the magnetic equatorial plane.

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Citations
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Journal ArticleDOI

Spatio-temporal structure of storm-time chorus

TL;DR: In this article, a sine-wave parametric model with a variable amplitude was used to analyze the lower band of chorus below one half of the electron cyclotron frequency, measured at a radial distance of 4.4 Earth's radii, within a 2000 km long source region located close to the equator.
Journal ArticleDOI

Global distribution of whistler‐mode chorus waves observed on the THEMIS spacecraft

TL;DR: Li et al. as discussed by the authors performed a global survey of whistler-mode chorus waves using magnetic field filter bank data from the THEMIS spacecraft with 5 probes in near-equatorial orbits, which confirmed earlier analyses of the strong dependence of wave amplitudes on geomagnetic activity, confinement of nightside emissions to low magnetic latitudes, and extension of dayside emissions to high latitudes.
Journal ArticleDOI

Global distribution of wave amplitudes and wave normal angles of chorus waves using THEMIS wave observations

TL;DR: In this paper, the global distribution of chorus wave amplitudes and their wave normal angles was investigated using high-resolution wave spectra and waveform data from THEMIS for lower-band and upper-band chorus separately, and it was shown that large amplitude chorus (>300 pT) occurs predominantly from premidnight to postdawn and is preferentially observed at lower L shells (50 pT).
Journal ArticleDOI

Global model of lower band and upper band chorus from multiple satellite observations

TL;DR: In this paper, the authors present a global model of lower band (0.1fce < f < 0.5fce), where fce is the local electron gyrofrequency, using data from five satellites, extending the coverage and improving the statistics of existing models.
References
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Limit on stably trapped particle fluxes

TL;DR: The limit on stably trapped particle fluxes determined theoretically and compared with data from Explorer satellites was first established in this paper, and the limit was later confirmed by the International Journal of Astronautics.
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The theory of plasma waves

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An investigation of whistling atmospherics

TL;DR: In this article, the authors investigated the nature and origin of whistlers, which are sometimes observed at frequencies below 15 kc/s and were found to follow the lines of force of the earth's magnetic field.
Journal ArticleDOI

Two types of magnetospheric ELF chorus and their substorm dependences

TL;DR: In this paper, the distribution of extremely low frequency (10-1500 Hz) magnetospheric chorus to all local times and latitudes is investigated in order to determine dependence on substorms, and to evaluate the conditions under which chorus is generated.
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