RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 12, ES5003, doi:10.2205/2012ES000522, 2012


Table 2. The Data on Recognition of TW-Disturbances
$i_{1}$ NDBC $i_{2}$ NDBC $i_{1}$ GC RAS $i_{2}$ GC RAS $\alpha_{lR}$
1 661,933 665,749 662,000 664,782 0.91
2 1,000,907 1,002,656 1,000,500 1,001,032 0.51
3 6,706,714 6,708,195 6,706,750 6,707,532 0.61
4 7,574,954 7,575,038 7,577,250 7,577,282 0.99

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Citation: Getmanov V. G. (2012), Method of spectral-time analysis for recognition of anomalies in time series with Raleigh- and tsunami-wave disturbances in signals from hydrostatic pressure sensors of ocean bottom seismic stations, Russ. J. Earth Sci., 12, ES5003, doi:10.2205/2012ES000522.


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