Narrow bursts of intense electron precipitation fluxes within inverted-V events

Inverted-V events have been examined in detail to identify small scale structures within them which might be related to auroral arcs. The rate of energy deposition into the atmosphere by the precipitating electrons of inverted-Vs was computed from the energy spectra measured by the AE-D satellite for 30 passes. Bursts of high deposition rate with a short duration (<5 seconds) were found inside inverted-V events. From an examination of 45 bursts, most bursts were found to have a latitudinal width less than 0.2°, and occurred from 65° to 75° invariant latitude during the evening hours (19-01 MLT). Optical emission intensities of 5577 A and 6300 A were inferred from the measured electron fluxes to show these bursts capable of producing bright emissions. These results suggest that the electron fluxes of these narrow bursts have the proper characteristics to cause discrete auroral arcs in the atmosphere.

[1]  R. Lysak,et al.  Satellite measurements and theories of low altitude auroral particle acceleration , 1980 .

[2]  G. Shepherd,et al.  An empirical determination of the production efficiency for auroral 6300‐Å emission by energetic electrons , 1980 .

[3]  R. Hoffman,et al.  Fluctuations of inverted V electron fluxes , 1979 .

[4]  B. A. Whalen,et al.  Do field-aligned auroral particle distributions imply acceleration by quasi-static parallel electric fields? , 1979 .

[5]  G. Shepherd,et al.  Energy transfer from excited N2 and O2 as a source of O(1S) in the Aurora , 1979 .

[6]  R. A. Hoffman,et al.  Characteristics of the inverted‐V event , 1979 .

[7]  B. Solheim,et al.  An indirect mechanism for the production of O(1S) in the aurora , 1979 .

[8]  C. Meng Electron precipitations and polar auroras , 1978 .

[9]  R. Arnoldy,et al.  Correlation of ground-based and topside photometric observations with auroral electron spectra measurements at rocket altitudes , 1977 .

[10]  J. Winningham,et al.  Simultaneous observations of discrete and diffuse auroras by the Isis 2 satellite and airborne instruments , 1976 .

[11]  R. Hoffman,et al.  Characteristics of auroral electron acceleration regions observed by Atmosphere Explorer C , 1976 .

[12]  D. Croley,et al.  Electron pitch‐angle distributions in an inverted ‘v’ structure , 1976 .

[13]  A. Vampola,et al.  Electron fluxes and correlations with quiet-time auroral arcs. Interim report , 1975 .

[14]  J. Burrows,et al.  On the angular distributions of electrons in ‘inverted v’ substructures , 1975 .

[15]  R. Arnoldy,et al.  Field‐aligned auroral electron fluxes , 1974 .

[16]  Andrew F. Nagy,et al.  A new model for the interaction of auroral electrons with the atmosphere: Spectral degradation, backscatter, optical emission, and ionization , 1974 .

[17]  C. Chappell,et al.  Twin payload observations of incident and backscattered auroral electrons , 1973 .

[18]  R. Hoffman,et al.  Low-energy electron experiment for Atmosphere Explorer-C and -D , 1973 .