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Across our comparisons, likelihood estimates of Ne that jointly estimated m were much smaller than other estimators that assume closed populations (Table 5 and 6).
The tsunami heights anywhere are also synthesized or forecasted from the estimated m.
When the estimated M w is reliable, the scaling law used is secondarily important.
The estimated M 7.1 fault plane is just located along the aftershock distribution (Fig. 4).
We derived D max and Dα of H-range above estimated M m = 2.195 (Table 4).
Table 4 also provides D max and Dα of H-amplitude and SI+SSC values above estimated M m = 1.180.
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There are also analytic and bootstrap bias-corrected ML estimators for estimating m that improve conventional ML estimators [5].
To find genes with significant expression changes between treatments, empirical Bayesian statistics were applied to the data by moderating the standard errors of the estimated M-values.
From the estimated M-matrix, we derived the relative change in R0 as outlined in the methods section.
To find genes with significant expression changes between groups, empirical Bayes statistics were applied to the data by moderating the standard errors of the estimated M-values.
The difference was seen in the estimated m-probabilities, with an increase in the estimates corresponding to year, month, day of birth and SSN and a decrease in estimates corresponding to telephone, zip code and sex compared to the conditional independence model.
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