Conclusions from cross-sectional data analysis



ITEM

Summary

ITEM Extrapolation of mean annual migration rates leads to an underprediction of population stability. This is because in a heterogeneous population, the individuals who are most likely to move, and who contribute to the mean annual migration rate will have moved away, leaving behind those who are less likely to move.

ITEM Cross-sectional analysis of this data set does not indicate any systematic variation of the mean migration rate with time. Even for data sets which showed evidence of temporal variation, there would be no indication of whether this was due to age, cohort or inertial effects.

ITEM Even though the standard Poisson model seems misspecified, because all the explanatory variables are exogenous the parameter estimates are consistent, ie. they tend to the true values when sample size is increased. However, standard errors are underestimated and may lead us to conclude that an explanatory variable is significant, when in fact it is not. For instance, results for the standard Poisson model suggest that educational qualifications do affect the likelihood of migration; the Poisson mixture model does not indicate significant educational qualification effects.

ITEM There is evidence that the likelihood of migration varies markedly between individuals and that the sample contains a number of "stayers", individuals likely never to move.

ITEM With a single count of outcomes for each individual, it is impossible to distinguish between a heterogeneous population, with some individuals having a consistently high and others a consistently low propensity to migrate, and a truly contagious process, in which an individual's experience of migration per se increases the probability of subsequent migration.


It is clear that the analysis of the cross-sectional data has answered only a few of the substantive questions of interest. No light has been shed on the dynamics of the migration process.
Longitudinal data analysis of individual event histories is necessary to explore the temporal variation in individual migration rates and to identify, for example, inertial effects.

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