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In the multivariate model of ≥3 mm reported displacements in weeks 1 and 2, lower age, moderate risk group, treatment verification with film and an increased number of fractions imaged were significant.
In the univariate, multivariate and stepwise models of ≥5 mm reported displacements there was evidence of an increased likelihood of a displacement across weeks 1 2 and 3 6 with film and an increased number of fractions imaged.
In the univariate models of ≥3 mm reported displacements in weeks 1 and 2 (Table 3), there was evidence of an increased likelihood of a displacement being reported with higher T-stage, lower age, moderate risk group, beam modification with LMPA, treatment verification with film, four phase I fields and increasing number of imaged fractions reported.
The proportion of reported displacements in a given treatment week is summarised in Fig. 2.
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Of the 34 protected areas included in the study, 26 reported displacement of people to make way for conservation, 21 reported conflicts between park management and communities, and 18 said they were not consulted before the protected areas were created.
For these reasons the models focused on the reporting of one reported displacement or more rather than the actual number of displacements.
In weeks 3 6 (Table 4), only an increasing number of fractions reported and treatment verification with film were associated with increased occurrence of at least one reported displacement.
Film verification increased the likelihood of at least one reported displacement compared with EPI, despite the fact that film was associated with significantly fewer displaced fractions reported than EPI and fewer images taken during treatment than EPI.
One in seven surveyed residents reporting displacement stated that some form of landlord harassment or discrimination – such as verbal abuse and threats, tampering with cars or utilities or withholding maintenance – contributed to their being uprooted.
In this paper, we report displacement rates on the seafloor surface and discuss interplate coupling along the Nankai Trough during the period before the 2011 Tohoku-oki earthquake and, thus, unaffected by postseismic effects from this enormous event.
In addition to the overall island displacement, studies of local displacement have reported new displacement phenomena.
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