There was no statistically significant main effect of elevation θ, F(4, 1440) = 2.55, p = 0.037; a statistically significant main effect of azimuth ϕ, F(11, 1440) = 1007.22, p < 0.0001; and no significant main effect of material, F(3, 1440) = 2.50, p = 0.053, α = 0.01, on ϕ̂ settings. There was a significant two-way interaction of θ and material, F(12, 1440) = 2.99, p < 0.0001. The remaining two-way and the three-way interactions were not significant.
Although not all paired comparisons were significant, post hoc analysis of the main effect “azimuth” indicated that ϕ̂ increased systematically and significantly with increases in ϕ. The differences between levels of ϕ̂ were significant except between pairs ϕ = −90 and ϕ = −60 and ϕ = −60 and ϕ = −30, α = 0.05, adjusted for multiple comparisons using Scheffe's S procedure. ϕ̂ means (−180.43, −143.84, −115.01, −56.64, −37.83, −5.24, 29.34, 67.94, 153.59) were not significantly different from the respective true ϕ values (−180, −150, −120, −60, −30, 0, 30, 60, 150). Azimuth estimates for ϕ = −90, 90, and 120 were significantly different from true ϕ values, ϕ̂ = −78.38, (t[139] = 4.29, p < 0.0001), ϕ̂ = 108.64, (t[139] = 5.68, p < 0.0001), ϕ̂ = 131.57, (t[139] = 3.407, p < .001), (one sample t tests, two-tailed, Bonferroni corrected α = 0.0042).
Following up the interaction of
θ and material on
ϕ̂ (see
Table 4) with a two-way ANOVA yielded no significant main effects of
θ and material on
ϕ̂ and no significant interaction.