People have already recognized the temperature increase anomaly before
earthquakes, and studies have been made on this phenomenon (WU, 1980;
WU et al., 1982; GENG, 1985). With the method of fixed-point network
observation, only the timing temperature data limited to some sites ca
n be obtained instead of dynamic evolution data of the temperature in
a large area within the seismogenic range. However, it is advantageous
to use the thermal infrared (IR) radiation measured by Meteosat to de
tect the ground temperature, because of the data accuracy, large area
coverage, large amount of information, and the capability of capturing
the time-space dynamic variation of the temperature increase before e
arthquakes. However relevant works on the relationship of the thermal
IR anomaly measured by Meteosat to seismic activity are only found pub
lished in the Soviet Union (GORNUY et al., 1988). The authors used the
thermal IR anomaly measured by Meteosat to monitor and tried to predi
ct the earthquake of October 18, 1989 in Datong, Shanxi Province and o
ther shocks, and obtained preliminary ideas and methods for carrying o
ut predictions in this way.