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Data collected from nine independent meteorological stations were compared with estimates from the nearest grid points of the Virtual Climate Station Network created by the New Zealand National Institute of Water and Atmospheric Research NIWAandalsoalso to estimates from NIWA's nearest actual meteorological stations.
For comparison to other studies that have used estimates from the nearest exposure monitoring location, we also calculated the monthly average PM2.5 from the nearest USEPA AQS monitoring location for all addresses 2000 2006.
In sensitivity analyses using average annual PM2.5 exposure estimates from the nearest U.S. EPA AQS monitor in 2000, as opposed to PM2.5 estimates from the time-varying geospatial model, the risks of all-cause mortality (HR = 1.35; 95% CI, 1.08 1.69) and fatal CHD (HR = 1.47; 95% CI, 0.73 2.99) were attenuated but elevated.
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Remaining genetic positions were estimated from the nearest flanking markers in the linkage map, assuming a linear relationship between genetic and physical positions over the interval.
However, (D_{c} ll 0.1 {text{m}}) is much smaller than the value (1 m) estimated from the near-fault seismic waveforms by Fukuyama and Suzuki (2016).
The DiD estimates from the two nearest neighbor matching show that in terms of magnitude the effect is about 5/100 of a standard deviation.
Marshall et al. (2008) reported correlations and κ-coefficients for estimates from the nearest-AQMS model (within 10 km) and estimates stemming from either an LUR (r = 0.61, κ = 0.42) or a dispersion model (r = 0.37, κ = 0.22).
Therefore, for these patients, ANC estimates were interpolated from the nearest two known ANC values.
Tree survival probability is estimated from the Knn nearest neighbors.
Moreover, these previous studies relied on exposure estimates based on data from the nearest regulatory air quality monitor, which do not capture within-city exposure contrasts adequately, possibly resulting in misclassification of exposure and reduced risk estimates (Woodruff et al. 2009).
The dip angle is difficult to estimate from the seismicity near the epicentral region, because it is distributed over a broad range due to its occurrence at the margin of two faults (the Hinagu and Futagawa faults; see line E E′ in Fig. 3).
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