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Monitoring of radiation background in the near-surface atmosphere and ofgamma rays, geoacoustic emission, and temperature in a borehole at 40m depth,as well as Doppler sounding on a low-inclined radio pass proceed at the TienShan mountain station (3340m a.s.l.) in Northern Tien Shan with common goal tosearch for seismogenic effects preceding earthquake. The flux of gamma rays inthe borehole varies negligibly between the days, and it is not influenced byprecipitations. Characteristic bay-like drops of the gamma ray flux were found(2-8)days before the M5.0-M6.2 earthquakes. In a M4.2 earthquake event with the5.3km epicenter distance anomalies were detected (7-10)days before theearthquake in variation of the gamma ray flux, geoacoustic emission, andtemperature. Simultaneously with gamma rays, a disturbance was detected in theDoppler shift of the ionospheric signal. Similarly, ionosphere disturbancestriggered by the growth of radioactivity in the near-surface atmosphere werefound at retrospective analysis of the Doppler shift data acquired afterunderground nuclear explosions at the Semipalatinsk testing site. This effectis considered from the viewpoint of the lithosphere-atmosphere-ionospherecoupling concept.

Monitoring of Gamma Radiation Prior to Earthquakes at a Study of Lithosphere-Atmosphere-Ionosphere Coupling in Northern Tien Shan