Atellitic thermal infrared brightness temperature anomaly image—short-term and impending earthquake precursors

1999 ◽  
Vol 42 (3) ◽  
pp. 313-324 ◽  
Author(s):  
Zuji Qiang ◽  
Changgong Dian ◽  
Lingzhi Li ◽  
Min Xu ◽  
Fengsha Ge ◽  
...  
Keyword(s):  
Brightness Temperature ◽  
Temperature Anomaly ◽  
Thermal Infrared ◽  
Earthquake Precursors ◽  
Short Term ◽  
Infrared Brightness

scholarly journals Efficient radiative transfer model for thermal infrared brightness temperature simulation in cloudy atmospheres

2020 ◽  
Vol 28 (18) ◽  
pp. 25730
Author(s):  
Wenwen Li ◽  
Feng Zhang ◽  
Yi-Ning Shi ◽  
Hironobu Iwabuchi ◽  
Mingwei Zhu ◽  
...  
Keyword(s):  
Radiative Transfer ◽  
Brightness Temperature ◽  
Thermal Infrared ◽  
Radiative Transfer Model ◽  
Transfer Model ◽  
Infrared Brightness

scholarly journals Kernel-driven model fitting of multi-angle thermal infrared brightness temperature and its application

2012 ◽  
Vol 30 (4) ◽  
pp. 361-365 ◽  
Author(s):  
Jing-Jing PENG ◽  
Qiang LIU ◽  
Qin-Huo LIU ◽  
Jia-Hong LI ◽  
Hong-Zhang MA ◽  
...  
Keyword(s):  
Brightness Temperature ◽  
Model Fitting ◽  
Thermal Infrared ◽  
Infrared Brightness

Alarm systems based on a pair of short-term earthquake precursors

1988 ◽  
Vol 78 (4) ◽  
pp. 1538-1549
Author(s):  
Giuseppe Grandori ◽  
Elisa Guagenti ◽  
Federico Perotti
Keyword(s):  
Statistical Analysis ◽  
Active Region ◽  
Southern California ◽  
Main Shock ◽  
Weak Shock ◽  
Earthquake Precursors ◽  
Alarm System ◽  
Short Term ◽  
Alarm Systems

Abstract A statistical analysis of the foreshock-main shock correlation for a seismically active region in Italy is presented. It is found that the probability that a weak shock be followed within 2 days by a main shock is of the order of 2 per cent, while the probability that a main shock be preceded by a foreshock is of the order of 50 per cent. These results are quite similar to those found by L. Jones (1985) for southern California. The effectiveness of alarm systems based on a pair of short-term earthquake precursors is then analyzed. In particular, the analysis shows under what conditions the precursor, consisting of potential foreshocks, could be combined with another precursor to provide a reasonably effective alarm system.

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