Using these values and related statistics, the optimization model estimated correction constants, called decision variables, that minimized the among-group variance of the adjoining strips.
The results of higher level calculations on smaller clusters were used to estimate corrections to the MP2/6-31G*//HF/6-31G* energies.
The strategy of using data linkage to estimate correction factors to improve Aboriginal identification in both the HMDC and mortality records has some limitations.
We estimated station corrections after applying the correction for abnormal seismic intensity distribution and adjusting M as previously described.
Furthermore, this method seems less sensitive to mismatched attenuation correction, erroneous normalization, and poorly estimated scatter correction, but such robustness also depends on the time resolution of the TOF-PET scanner [16 18, 20, 21].
In addition, when estimating station corrections, we applied corrections of the abnormal seismic intensity distribution and source term for Eq. (2) in order to reduce the effects of factors other than site amplification.
The estimated error-correction term measures the speed of short-run adjustment to long-run equilibrium after an exogenous shock.
In this paper, we discussed the improvement in the expectation of seismic intensity by replacing ARV by an empirically estimated station correction.
However, if a similar filling percentage can be assumed as the one previously estimated, a correction factor of slightly larger than 2 should be included.
