Chepasov V.I., Nikonorova О.А., Kuryakova Т.А., Teterin А.P. EARTHQUAKE FORECAST BASED ON THE PERIODS OF HARMONICS WITH THE MAXIMUM AMPLITUDE OF EARTHQUAKE LOCAL TIME, EARTHQUAKE DAYS, TIDAL VARIATIONS IN GRAVITY [№ 4 ' 2009] On the basis of spectrum analysis, the periods of harmonics with the maximum amplitude for earthquake local time, earthquake days, parameters of tidal variations in gravity during events were identified. With the aid of found periods of harmonics with the maximum amplitude a methodology is suggested to forecast earthquake time through cumulative sum calculation starting from 1987 (in hours).
Kuryakova Т.А., Teterin А.P., Kaykova Т.V. SPECTRAL CONDITIONALITY OF SOIL PARAMETERS [№ 12 ' 2008] The article provides an analysis of the spectral and quantitative causation of the humus for the two time reckonings. The analysis result are given for the normalized research matrixes and for the ranked normalized research matrixes.
Kuryakova T.A., Nepsha A.A., Teterin A.P. SPECTRAL FORECAST OF SOIL PARAMETERS [№ 11 ' 2008] The authors study methods of spectral forecast of soil parameters using unranked and ranked normalized investigation matrices built for different time counts.
[№ 10 ' 2008]
Chepasov V.I., Osipov O.V., Teterin A.P. MISTAKE OF SIGNALS APPROXIMATION AT TIME AND SPECTRAL SPHERES [№ 4 ' 2008] The results of signals approximation at time and spectral spheres are regarded in this article. Polynomial models of parametritic forecasting got with method of the least square and with method of Brandon D. At time and spectral spheres are given here.
Chepasov V.I., Teterin A.P., Osipov O.V. FORECAST OF EMERGENCY CALL NUMBER AT TIME AND SPECTRAL SPHERE [№ 2 ' 2008]
Chepasov V.I., Osipov O.V., Teterin A.P. ALGORITHMIC AND PROGRAM REALIZATION OF CONSTRUCTION OF OPTIMAL FORECAST MODELS [№ 1 ' 2008] Methodic of forecasting models finding with minimal number of forecasting mistakes is regarded in this article. Polynomial models of parametric forecast and algorithmic scheme of optimal forecast models search are the base of methodic.
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