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Thickness estimates also have direct application in mineral exploration and seismic risk assessment.
Thickness estimates are often highest in parietal (particularly superior parietal) and occipital cortices.
Aquifer thickness estimates based on resistivity data were significantly improved as a result.
This is reflected in the thickness estimates which show increasing variance with the degree of corrosion.
Comparison between measures of relief and ice thickness estimates indicates that relief production in glaciated mountain belts scales with ice thickness and consequently also drainage area.
Regional thickness estimates were highly consistent across regions, as shown by the low mean deviation (between scans) for each region in Fig. 2.
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Figure 2 displays the relationship between the mean macular sensitivity as a function of retinal thickness estimated by a LOWESS smooth function (thick gray line) for normal participants as well as those with uveitis and no macular edema.
Figure 1 displays the relationship between the mean macular sensitivity as a function of retinal thickness estimated by a locally weighted scatterplot smoothing (LOWESS) smooth function (thick gray line).
Maximum thickness estimated was 1.1 km (Fig. 8(b)).
The film thickness estimated from ellipsometry experiments was 200 nm for both samples.
Of course, a thickness estimate can still be done from the G band intensity.
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