Satellite observations of VLF emissions and their association with energetic charged particles.
Intensity and occurrence of VLF emissions and charged particle fluxes, using Injun 3 satellite observations
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Intensity and occurrence of VLF emissions and charged particle fluxes, using Injun 3 satellite observations
Ionospheric DC electric fields long period oscillations at high latitudes observed by polar orbiting Injun 5 satellite
Because predicted relationship (epsilon directly varies with V squared) between auroral electron energy flux (epsilon) and the inferred acceleration potential drop (V) for accelerated Maxwellian distributions was favorably tested by other using sounding rocket data for the limiting case of eVE 1 (where Ec is the characteristic energy of the accelerated Maxwellian distribution) and for a single inverted-V observed by the Injun 5 satellite, data from Atmosphere D were used to extend these studies over the range .2 eV/Ec 5 and for a wide range of latitudes and local times on both the nightside and the dayside. Results show good agreement with the full accelerated Maxwellian model. An analytical approximation to the electron energy flux was derived which better describes the data over the range .2 eV/Ec approximated 3. Analyses of individual energy spectra at small and large pitch angles through well-defined inverted-V structures suggest that the altitude of the inferred potential drop maximizes near the center of the inverted-V's.
The basic theory of solar flux attenuation by the earth's atmosphere is reviewed and a model of the time-varying flux observed by a satellite during eclipse passage developed. The general model is applied to the specific problem of variations in photoelectron flux during penumbral passage and the effects of wavelength, solar activity, and atmospheric constituents on photoelectron emission investigated. Predictions of the photoelectron current expected from tungsten and aluminum surfaces are then successfully compared with actual observations from the ATS-5 and Injun 5 satellites confirming the validity of the model.
This paper presents a study of auroral-zone vlf hiss and low-energy charged-particle observations with the Injun 5 satellite. The results of this study provide a direct verification of the association between auroral-zone vlf hiss and intense fluxes of low-energy electrons with energies on the order of 100 eV to several keV. On the dayside of the magnetosphere, these low-energy electrons are identified with the dayside polar-cusp region observed at higher latitudes with the Imp 5 satellite. At other local times, through the dawn and dusk regions and into the nightside of the magnetosphere, the vlf hiss and low-energy electron precipitation regions are believed to correspond to the extension of the dayside polar cusp into the distant plasma sheet and downstream magnetosheath on the nightside of the magnetosphere. Intense fluxes of upgoing electrons are often observed in a narrow latitudinal band near the low-energy electron precipitation bands. These upgoing electrons are believed to be associated with another type of vlf emission called a saucer, which is frequently observed with Injun 5.
This paper presents a series of simultaneous observations of very-low-frequency radio noise by the Injun 5 satellite and of visual aurora along the same geomagnetic-field line by the Fort Churchill Auroral Observatory. Seven observations from the period of August 29, 1968, to March 4, 1969, are discussed. In 5 of the 7 events studied vlf hiss is observed in association with auroral-light emissions. These observations typically show the occurrence of vlf hiss in the general region of the auroral arc, with significant changes in the vlf spectrum sometimes observed in the immediate vicinity of the auroral arc. One event for which the associated charged-particle fluxes have been analyzed is investigated in detail. The vlf radio noise intensity for this event is among the largest observed with Injun 5 and is much greater than can presently be explained by an incoherent Cerenkov radiation mechanism.
Diurnal variation of the geomagnetically trapped radiation
Solar energetic particle intensities obtained with Mariner IV and Injun IV during 5-12 February 1965 cosmic ray event
Simultaneous observations of solar protons inside and outside magnetosphere by Explorer XXXIII AND Injun IV
Low energy trapped proton observations with Injun 4 satellite
Injun 3 satellite spectrophotographic analysis of VLF noise emissions during magnetic storms, and assessment of relationship between variations in emission and energetic electron fluxes
Auroral zone electron microbursts observed with Injun 3 satellite, discussing time profiles and relation to X ray microbursts
Injun 3 satellite observations reveal electron microbursts association with VLF chorus emission
Low energy geomagnetically trapped proton intensities from high latitude orbiting Injun 4 satellite observations
Protons emitted by July 7, 1966 solar flare observed by low altitude high latitude Injun 4 satellite
Ion cyclotron whistler in very low frequency noise observations with Injun 5 satellite
VLF Poynting flux measurement technique used on Injun 5 satellite
Ion cyclotron whistler in Injun 5 satellite VHF radio noise data