Attenuation of decameter wavelength sky noise during x-ray solar flares in 2013-2017 based on the observations of midlatitude HF radars

被引:22
作者
Berngardt, O. I. [1 ]
Ruohoniemi, J. M. [2 ]
Nishitani, N. [3 ]
Shepherd, S. G. [4 ]
Bristow, W. A. [5 ]
Miller, E. S. [6 ]
机构
[1] Inst Solar Terr Phys SB RAS, 126a Lermontova Str, Irkutsk 664033, Russia
[2] Virginia Tech, 302 Whittemore, Blacksburg, VA 24061 USA
[3] Nagoya Univ, Inst Space Earth Environm Res, Chikusa Ku, Furo Cho, Nagoya, Aichi 4648601, Japan
[4] Dartmouth Coll, 14 Engn Dr, Hanover, NH 03755 USA
[5] Univ Alaska Fairbanks, 903 Koyukuk Dr, Fairbanks, AK 99775 USA
[6] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD USA
基金
日本学术振兴会;
关键词
Ionospheric absorption; Noise level; Passive sounding; Midlatitude HF radars; IMAGING RIOMETER; RADIO PATHS; ABSORPTION; SUPERDARN; PROPAGATION;
D O I
10.1016/j.jastp.2018.03.022
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Based on a joint analysis of data from 10 midlatitude decameter wavelength radars effects are investigated during 80 x-ray flares that occurred in the period 2013-2017. For the investigation nine mid-latitude SuperDARN radars of the northern hemisphere (Adak Island West and East radars, Blackstone radar, Christmas Valley East and West radars, Fort Hays East and West radars, Hokkaido East radar and Wallops radar) and Ekaterinburg coherent decameter radar of ISTP SB RAS are used. All the radars work in the same 8-20 MHz frequency band and have similar hardware and software. During the analysis the temporal dynamics of noise from each of the radar direction and for each flare is investigated separately. As a result, on the basis of about 13000 daily measurements we found a strong anticorrelation between noise power and x-ray flare intensity, indicating that short-wave sky noise can be used to diagnose the ionospheric effects of x-ray solar flares. It is shown that in 88.3% of cases an attenuation of daytime decameter radio noise is observed during solar flares, and the attenuation correlates with the temporal dynamics of the solar flare. The intensity of decameter noise anticorrelates well (the Pearson correlation coefficient better than -0.5) with the shape of the X-ray flare in the daytime (for solar elevation angle > 0) in 33% of cases, the average Pearson correlation over the daytime is about -0.34. Median regression coefficient between GOES 0.1-0.8 nm x-ray intensity and daytime sky-noise attenuation is about - 4.4.10(4) [dB.m(2)/Wt]. Thus, it is shown that measurements of the sky noise level at midlatitude decameter radars can be used to study the ionospheric absorption of high-frequency waves in the lower ionosphere during x-ray solar flares. This can be explained by the assumption that the larger part of the decameter sky noise detected by the radars is produced by ground sources at distances of the first propagation hop (similar to 3000 km).
引用
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页码:1 / 13
页数:13
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