Study on Thermal Anomalies of Earthquake Process by Using Tidal- Force and Outgoing-longwave-radiation

نویسندگان

  • Xuedong ZHANG
  • Chunli KANG
  • Weiyu MA
  • Jing REN
  • Yong WANG
چکیده

Four earthquakes above M5.0 in Yunnan and Tibet, China occurred from 2010 to 2011. By calculating the tidal-force changes induced by celestial bodies in this region, we found that the earthquakes occurred when tidal forces continuously grew from low to peak levels and approached the maximum amplitude phase, which indicated a tidal force that had a trigger or inducing effect of active tectonic earthquakes when the ground stress reached a critical point. At the same time analyzing the abnormal changes of outgoing longwave radiation (OLR), along with the tidal cycle, indicated that the regional distribution of the enhancement region of OLR anomalies was closely related to geologic structure, especially active faults. The OLR radiation anomaly evolved as follows: an initial infrared rise, followed by an enhancement reaching peak, attenuation, and then a return to normal. The entire process was similar to changes observed in rockbreaking process under stress loads. Our investigation showed that the tidalforce changes caused by celestial bodies could trigger an earthquake when tectonic stress reached its critical breaking point, and the OLR anomaly was the radiation signature of the change in seismic tectonic stress. Therefore, the method of combining measurements of the tidal-force changes induced by celestial bodies with those of thermal-anomaly changes has some practical value for detecting the precursor state of impending earthquakes.

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تاریخ انتشار 2017