Diurnal and annual variations in 10-kHz radio noise

被引:9
作者
Clilverd, MA
Watkins, NW
Smith, AJ
Yearby, KH
机构
[1] British Antarctic Survey, Cambridge CB3 0ET, England
[2] Univ Sheffield, Dept Automat Control & Syst Engn, Sheffield S1 3JD, S Yorkshire, England
关键词
D O I
10.1029/1999RS900009
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
It is shown that the investigation of lightning activity levels, using very low frequency radio emissions near 10 kHz, needs to take into account the significant influences of subionospheric propagation. Ten-kilohertz spectral power measurements made at Halley, Antarctica (76 degrees S, 26 degrees W), show at least two significant periodicities. The largest variation (10 dB) is due to the diurnal cycle and is strongly dominated by South American thunderstorm activity levels. The effect of African thunderstorm activity is observable in the diurnal variation plots but is strongly reduced by disadvantageous propagation conditions. The analysis suggests that given two identical tropical source regions, one situated east and one situated west, of a polar receiver site, the region to the west will tend to dominate the diurnal variation. The smaller annual variation at Halley (3 dB) can be explained by the improved subionospheric propagation conditions during the Southern Hemisphere winter counterbalancing the seasonal effects of decreased source activity in South America.
引用
收藏
页码:933 / 938
页数:6
相关论文
共 19 条
[1]  
BULLOUGH K, 1968, J SCI I 2, V2, P77
[2]   Seasonal variations of globally measured ELF/VLF radio noise [J].
Chrissan, DA ;
FraserSmith, AC .
RADIO SCIENCE, 1996, 31 (05) :1141-1152
[3]   Ground-based evidence of latitude-dependent cyclotron absorption of whistler mode signals originating from VLF transmitters [J].
Clilverd, MA ;
Horne, RB .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1996, 101 (A2) :2355-2367
[4]   USE OF VLF TRANSMISSIONS IN THE LOCATION AND MAPPING OF LIGHTNING-INDUCED IONIZATION ENHANCEMENTS (LIES) [J].
DOWDEN, RL ;
ADAMS, CDD ;
COTTON, PD .
JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1992, 54 (10) :1355-1373
[5]  
GARDNER RL, 1990, LIGHTNING ELECTROMAG, P191
[6]   THUNDERSTORM MONITORING IN SOUTH-AFRICA AND EUROPE BY MEANS OF VERY LOW-FREQUENCY SFERICS [J].
GRANDT, C .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D16) :18215-18226
[7]  
GRUBER A, 1984, B AM METEOROL SOC, V65, P958, DOI 10.1175/1520-0477(1984)065<0958:TSOTNO>2.0.CO
[8]  
2
[9]  
*INT RAD CONS COMM, 1983, 3222 INT RAD CONS CO
[10]  
KESSLER A, 1986, HEAT BALANCE CLIMA A, V1