Day–night, seismic, and solar flare effect on the propagation of 24 kHz sub-ionospheric VLF transmitter signals

The preliminary results of a collaborative study on the amplitude variation of 24 kHz sub-ionospheric NAA VLF transmitter signals transmitted from Cutler, Maine (Lat. 44.6°N, Long. 67.2°W) and monitored simultaneously at Budapest (Lat. 47.5°N, Long. 19.17°E), Hungary and Agra (Lat. 27.2°N, Long. 78°...

Full description

Saved in:
Bibliographic Details
Published in:Physics and chemistry of the earth. Parts A/B/C Vol. 31; no. 4; pp. 416 - 421
Main Authors: Kumar, Manoj, Singh, Vikram, Singh, Birbal, Steinbach, P., Lichtenberger, J., Hamar, D.
Format: Journal Article
Language:English
Published: Elsevier Ltd 2006
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:The preliminary results of a collaborative study on the amplitude variation of 24 kHz sub-ionospheric NAA VLF transmitter signals transmitted from Cutler, Maine (Lat. 44.6°N, Long. 67.2°W) and monitored simultaneously at Budapest (Lat. 47.5°N, Long. 19.17°E), Hungary and Agra (Lat. 27.2°N, Long. 78°E), India are presented. The time segments of the propagation paths are so chosen that they lie in the post-midnight hours over Budapest and sunrise hours over Agra. The results show that the amplitude at Budapest decreases after midnight hours by about 3 dB whereas the same at Agra increases by 5 dB during sunrise normally. The anomalous enhancements and reductions in the amplitude variation during the three month period of July–September 2002 along Cutler–Agra great circle path (GCP) are examined in the light of seismic, solar flares, and magnetic storm effects. It is found that the occasional amplitude reductions are caused by earthquakes ( M > 5) which occurred along the GCP, and the enhancements are caused by solar flares. The magnetic storms do not seem to influence the data except in the case when associated with large solar flares.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ObjectType-Article-2
ObjectType-Feature-1
ISSN:1474-7065
1873-5193
DOI:10.1016/j.pce.2006.02.044