scholarly journals Magnetic aspect sensitivity of high-latitudeEregion irregularities measured by the RAX-2 CubeSat

2014 ◽  
Vol 119 (2) ◽  
pp. 1233-1249 ◽  
Author(s):  
H. Bahcivan ◽  
J. W. Cutler ◽  
J. C. Springmann ◽  
R. Doe ◽  
M. J. Nicolls
Keyword(s):  
2019 ◽  
Vol 16 (2) ◽  
pp. 211-215
Author(s):  
Haiyin Qing ◽  
Zhengyu Zhao ◽  
Yaohui Xu ◽  
Chen Zhou
Keyword(s):  

1960 ◽  
Vol 38 (5) ◽  
pp. 593-603 ◽  
Author(s):  
P. A. Forsyth

By assuming that auroral radio reflections are produced by volume scattering in clouds of ionization having the same spatial configuration as the visible auroral structures, and by taking into account the radar pulse duration and antenna beam width, it is possible to predict the probability of echo occurrence as a function of range and azimuth. This echo distribution is quite similar to that observed experimentally even when "aspect sensitivity" of the individual scatterer is neglected. Unfortunately, the optical evidence is not sufficiently extensive to permit precise calculations to be made, nor the radio evidence to permit detailed comparisons, but previous estimates of the shape of the scattering structures that have been based on the azimuthal echo distribution without regard to the factors discussed here are likely to be seriously in error.


Radio Science ◽  
2001 ◽  
Vol 36 (6) ◽  
pp. 1477-1492 ◽  
Author(s):  
Noriyuki Kawano ◽  
Shoichiro Fukao

2004 ◽  
Vol 4 (3) ◽  
pp. 685-692 ◽  
Author(s):  
Q. H. Zhou ◽  
Y. T. Morton ◽  
J. D. Mathews ◽  
D. Janches

Abstract. The aspect sensitivity of VHF echoes from field aligned irregularities (FAI) within meteor trails and thin ionization layers is studied using numerical models. Although the maximum power is obtained when a radar is pointed perpendicular to the field line (B), substantial power can be obtained off the B direction if the ionization trail/layer is thin. When the FAI length along B is 20 m, the power observed 6° off B is about 10 db below that perpendicular to the B direction. Meteoric FAI echoes can potentially be used to determine the diffusion rate in the mesopause region. Based on the aspect sensitivity analysis, we conclude that the range spread trail echoes far off B observed by powerful VHF radars are likely due to overdense meteors. Our simulation also shows that ionospheric FAI echoes can have an altitude smearing effect of about 4 km if the vertical extension of a FAI-layer is around 100 m, which has often been observed at Arecibo. The altitude smearing effect can account for the fact that the Es-layers observed by the Arecibo incoherent scatter radar are typically much narrower than FAI-layers and the occurrence of double spectral peaks around the Es-layer altitude in FAI echoes.


1972 ◽  
Vol 50 (21) ◽  
pp. 2557-2564 ◽  
Author(s):  
D. R. McDiarmid

Previous measurements of the aspect sensitivity of radio aurora at VHF have yielded two distinctly different values, namely, 10 dB/deg and 1 to 2 dB/deg. In this paper, a previously discussed event is re-analyzed in greater detail in an attempt to resolve this apparent anomaly. The results of this analysis, which takes account of the effects of a number of measurement errors and uncertainties, lead to the conclusion that the aspect sensitivity of the event could not have been greater than [Formula: see text] in the aspect angle interval of approximately 4.5° to 19.5°. The most likely value is between 1.3 and 1.5 dB/deg. It is suggested that the two observed aspect sensitivity curves correspond to different radio aurora producing mechanisms.


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