VLF noise during Forbush decreases of cosmic rays

被引:0
作者
Karimov, RR [1 ]
Mullayarov, VA [1 ]
Kozlov, VI [1 ]
机构
[1] Russian Acad Sci, Siberian Div, Inst Cosmophys Res & Aeron, Yakutsk 677891, Russia
关键词
D O I
暂无
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
The VLF-noise amplitude variations in Yakutsk during Forbush decreases of cosmic rays are considered by the. epoch superposition method. Nighttime VLF-noise amplitudes reflect mainly the activity of their thunderstorm source in the equatorial region (Africa): summer daytime amplitudes, local thunderstorms activity. Two effect phases can generally be distinguished with respect to the Forbush decrease onset. The VLF noise amplitude decreases by day 0 or -1 during the first phase and increases by day +1 or +2 in the second phase, exceeding the initial undisturbed amplitude on days -5 or -4.
引用
收藏
页码:393 / 395
页数:3
相关论文
共 11 条
[1]   Cosmic ray decreases: 1964-1994 [J].
Cane, HV ;
Richardson, IG ;
vonRosenvinge, TT .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1996, 101 (A10) :21561-21572
[2]  
DRUZHIN GI, 1986, GEOMAGN AERON+, V26, P258
[3]  
DRUZHIN GI, 1994, GEOMAGN AERON+, V34, P174
[4]  
DRUZHIN GI, 1988, GEOMAGN AERON+, V28, P81
[5]  
Krivoshapkin PA, 1997, GEOMAGN AERON+, V37, P128
[6]   THUNDERSTORMS, COSMIC-RAYS, AND SOLAR-LUNAR INFLUENCES [J].
LETHBRIDGE, MD .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D9) :13645-13649
[7]  
MULLAYAROV VA, 1995, GEOMAGN AERON+, V35, P143
[8]  
Mullayarov VA, 1997, GEOMAGN AERON+, V37, P132
[9]  
Mullayarov VA, 1999, GEOMAGN AERON+, V39, P110
[10]  
PUDOVKIN MI, 1992, GEOMAGN AERON+, V32, P1