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Growth and migration parameters were chosen to match results of clinical studies.
Buffer overflow and its relationship with migration parameters were investigated to resolve the issues of observed message buffer overflow and the loss of good solutions obtained from migration.
Modal values of the posterior probability distributions for the two migration parameters were consistent with very low levels of ongoing post-divergence migration between western (K1) and eastern (K3) Mediterranean populations, well below that often considered necessary for ecological or evolutionary trajectories to remain correlated [42].
Scaled migration parameters were all very close to zero.
When the MLEs for the migration parameters were transformed into population migration rates, 2Nem = m* θ/2) was estimated among the populations of different mountain ranges.
Migration parameters were estimated across all loci in terms of mutation-scaled immigration rates M (m/μ) and mutation-scaled effective population sizes Θ (4 Neμ) were calculated for each population, as implemented in Migrate-n v3.6 [ 71].
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When the MLE (maximum likelihood estimates) for the migration parameters are transformed into the population migration rates, M1 = 2 N1 m1 = m1* θ1/2) estimated from Japanese populations to the Chinese population in C. revoluta is higher than the estimate, M2 = 2N2m2 = m2* θ2/2), from China to Japan, i.e., 8.0134 vs. 0.5431 based on the combined data (Table 6).
However, the migration parameter was estimated to be 0.0417 (4Nm3→2) from the pooled tobacco populations to the Eastern NC potato population.
The boundary motion was measured in the regime between 330 °C and 415 °C, and the corresponding migration activation parameters were determined.
They further suggest that the velocity and persistence of DCs are two migration parameters that are differentially regulated and can be uncoupled by knocking down specific IP3R isoforms.
The first genealogy was started with a random tree, and initial theta and migration rate (M) parameters were obtained from F ST calculations.
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