RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 18, ES4001, doi:10.2205/2018ES000624, 2018
| Classical method | Sequential method | |
| 1 | 2 | |
| Normal distribution | ||
| $E_0 \nu = \displaystyle{\frac{ (u_{\alpha} + u_{\beta})^2 }{(\omega_1 - \omega_0)^2 / \sigma^2}}$ | $E_0 \nu = \displaystyle{\frac{(1 - \alpha)\ln B + \alpha\ln A}{(-0.5)(\omega_1 - \omega_0)^2 / \sigma^2}}$ | |
| Exponential distribution | ||
| $E_0\nu = \displaystyle{\frac{u_\alpha \omega_1 + u_\beta \omega_0}{\omega_1 - \omega_0}}$ | $E_0\nu = \displaystyle{\frac{(1- \alpha) \ln B + \alpha \ln A}{\ln(\omega_1 / \omega_0)(\omega_1 - \omega_0)/\omega_0}}$ | |
| Normal distribution | ||
| $E_1\nu = \displaystyle{\frac{(u_\alpha + u_\beta)^2}{(\omega_1 - \omega_0)^2/\sigma^2}}$ | $E_1\nu = \displaystyle{\frac{\beta \ln B + (1-\beta) \ln A}{0.5(\omega_1 - \omega_0)^2/\sigma^2}}$ | |
| Exponential distribution | ||
| $E_1\nu = \displaystyle{\frac{(u_\alpha \omega_1 + u_\beta \omega_0)^2}{(\omega_1 - \omega_0)^2}}$ | $E_1\nu = \displaystyle{\frac{\beta \ln B + (1-\beta) \ln A}{\ln(\omega_1 / \omega_0)(\omega_1 - \omega_0)/\omega_1}}$ |
Citation: Mkrtchyan F. A., S. M. Shapovalov (2018), Some aspects of remote monitoring systems of marine ecosystems, Russ. J. Earth Sci., 18, ES4001, doi:10.2205/2018ES000624.
Copyright 2018 by the Geophysical Center RAS.