Effects of nearby thunderstorms and earthquakes recorded on the Hyderabad magnetograms during the period January 1, 1965, to June 30, 1966, are discussed in the light of available literature.
The thunderstorm effect caused by the magnetic field of the lightning discharge currents appears as a sudden change (kick) of 2-10γ in
H or
D or both and sometimes 1-2γ in
Z also which is followed by very rapid oscillations decaying exponentially in 2-5 minutes.
Earthquakes of moderate and great intensity with epicentres in India and its neighbourhood produce characteristic effects on the Hyderabad magnetograms (
H,
D and
Z). The oscillations grow to a maximum of about 30γ in the middle of the effect and then die off gradually over 15-20 minutes. Sometimes the arrivals of seismic body waves P and S and the Rayleigh surface waves LR are clearly seen in the effects recorded on the magnetograms, indicating that the response of the variometers to earthquakes is primarily mechanical. However, a small amount of magnetic effect due to piezomagnetic fluctuations in the rocks underneath the observatory at the time of passage of earthquake waves seems to be inseparably mixed with the mechanical effect.
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