Go to Home Page

Forecasting Techniques
 
Forecast Techniques:
Although strides have been made in long-term seismic forecasts, studying the probability of an event in the next ten or thirty years, so far short-term earthquake forecasting has eluded the scientific community. Unfortunately, this short-term forecast is the one that is desperatly needed to save lives if we are to provide an early warning in weeks or days to potential victims of an impending destructive earthquake. However, science has indeed made huge strides in the forecast of other physical phenomena such as hurricanes or tornadoes.

Therefore, since earthquakes are physical phenomena, it can be expected that science will find some predictive qualities to forecast the behavior of seismic activity. The most promising area of research is seismo electromagnetic science, which monitors and analyses the subtle effects in the earth and ionosphere that occur several hours to several days before major earthquakes. This area of science may very well provide the foundation for earthquake forecasting.

Mechanical Monitoring Methods (Long Term, Decades-Years)
Most earthquake forecasting has focused on studying mechanical indicators in the recent past
  • Stress build up (GPS and INSAR monitoring of plate motion)
  • Strain Monitoring (Strain meters)
  • Seismicity rates (chaos theory, quake gap theory)

Electromagnetic Monitoring Methods (Short Term, Weeks-Days)
More recently, the International community has started to monitor Electromagneticsignals

The basis of this theory is that rocks near the hypocenter of the impending quake are stressed to their elastic limit and begin to crack --without actually displacing (rupturing) yet. This cracking process releases a flood of charged particles (some researchers say electrons, some say positive charge carriers called p-holes, and some simply say ionic water migrates through the cracks). These moving charges form huge underground currents (10^6 Amps estimated in the 1999 Chi-Chi, Taiwan quake) which disturb the Earth's normal magnetic field. These disturbances can be detected at ultra-low frequencies (ULF) due to the signal's ability to penetrate kilometers of solid rock only at low frequencies (electromagnetic skin effect). Some lab experiments have also shown that p-holes can migrate to the surface, drop their charges, and emit IR radiation in discreet frequencies bands (NASA-Freund) that have been detected by satellite IR instruments (NASA-Ouzounov). There are other electromagnetic effects (see below).

 
[ Home ] - [ About ] - [ Reserach ] - [ News ] - [ Data ] - [ Services ] - [ Community ] - [ Contact ]
© 2008 QuakeFinder, LLC.