Mogi (1973) found that the seismic activity trends to progress in time from a shallow to a deep region within a descending lithosphere in the Mariana and Tonga arcs and the rate of migration is estimated at about 50 km per year.
Maximal slope of migration was estimated over a 10-min interval.
Migration was estimated based on the change in population between 1970 and 2009 using a stable in-migration among men and an increasing in-migration among women.
Very low migration among populations was estimated for subset 1 (Nem: 0.05 to 0.31, Table 5), but for the more detailed subset 2, higher asymmetrical migration was estimated within the GBR (mean Nem up to 3.03, Table 6).
Thus, migration was estimated to be solely restricted by water levels in PAL at 734.9 - 735.2 m a.s.l. in the gates, and 722.4 - 726.4 m a.s.l. in the tunnel.
The FV i.e. loss from a country through migration was estimated as: FV = Sum * (1+r)n where; Sum = amount invested; r = compound interest rate; n = the number of years the money is invested.
Migration is estimated to be more frequent from population C to population RL (3.86445 vs. 41.10288, cpDNA, and 2.25430 vs. 48.99630, mtDNA), contributing to the lack of genetic differentiation between populations, as indicated by Fst values of 0.0056 (cpDNA) and 0.021 (mtDNA) [cf. [ 55]].
Since migrations occur as a movement of biomass through large parts of water column, the CLEAN spectral and autocorrelation analyses were applied to each depth layer independently (figure 1), thus enhancing the spatial and temporal resolutions with which the periodicity of these migrations were estimated (see the electronic supplementary material).
This is excellent news.Net migration (immigration minus emigration) is estimated to have reached 212,000 in the year to last September.
Migration rates were estimated from photomicrographs of migration assays taken at time point 0 hours and time point 24 hours [ 13].
