On 27 August 1998, at 10:22 UT, an extremely intense gamma ray Rare passed
through the solar system. The gamma -ray burst lasted only 5 min and result
ed in the ionization of a large portion of the Earth's night-side upper atm
osphere to levels found normally only during the daytime. During this perio
d we were continuously monitoring extremely low frequency (ELF) electromagn
etic waves in the range 1-50 Hz, at a new monitoring site established in th
e Negev Desert, Israel. We have analysed our ELF data, including the Schuma
nn resonances, during this period, and no noticeable changes in the ELF sig
nals are observed as a result of this event. This is very different to obse
rvations in the VLF range that showed extreme changes in amplitude and phas
e resulting from this gamma -ray burst. Theoretical modeling points to thre
e factors that can explain the differences between the VLF and ELF signal r
esponses. (i) different properties of the ELF and VLF signals within the ti
me scale of the gamma -ray burst; (ii) different paths of these signals dur
ing the event; and (iii) the different influences of the day/night asymmetr
y on the propagation of ELF and VLF waves. (C) 2001 Elsevier Science Ltd. A
ll rights reserved.