Addendum to :
Hupé, J.M., & Rubin, N. (2003) The dynamics of bi-stable alternation in ambiguous motion displays: a fresh look at plaids. Vision Research 43: 531 - 548.
RTtransp is a new and reliable measure of the
probability of coherence in plaids. Since each measure is relatively
fast to obtain
(as long as the parameters are chosen so the probability of seeing the
transparent percept is not too low), it is possible to test many
parameters simultaneously within one experiment, using full-factorial
designs. Such designs have also the methodological advantage of
presenting to the observer many different stimulus configurations, so
the observer cannot guess what the effects of the manipulated variables
are while running the experiment (as long as the stimuli are presented
in a random order, of course). Linear analyses are a
powerful tool to study the effects of many variables. But their
reliability depend on two major assumptions: that the noise in the data
be normally distributed, and that the variances be homogenously
distributed. RTtransp values have a
log-normal distribution, so transforming them to their natural log
allows us to use linear model analyses (see paper). The homogeneity of
variances assumption can be checked in several ways. When doing a
simple ANOVA, one can compare the variances of the different groups,
and test if they are significantly different from each other. However,
these tests do not indicate which group(s) is/are significantly
different from the others, and we can not use them when several
variables are tested, some of them being linear predictors (or
covariates). A convenient way of visualizing the homogeneity of
variances is to plot the residuals as a function of the values
predicted by the linear model :
Figure 1
In the case presented in Figure 1, there is no
obvious reason to suppose that the variances are different in the four
different groups
– the visual inspection can be confirmed here by doing a test of
homogeneity of variances (p = 0.60, Hartley, Cochran, Bartlett).
Residual plots allow us to check easily if there is any systematic
relationship between the effects of parameters and variance. For
instance, if we had not transformed the data to their natural log for
the data presented in Figure 1, we would have observed that the
variance systematicaly increases for larger predicted values of
RTtransp
:
Figure 2
Inspection of residuals plots allows us therefore to
verify easily to what extent the conditions of validity of the linear
model
analysis were respected. Moreover, residuals plots can be generated
whatever
the complexity of the linear model – while in that case it does not
allow
to verify that the variances are homogenous between any pair of groups,
it
makes possible to detect any systematic bias in the data, as we can now
observe
for the analysis of the data of Experiment II presented in the paper.
Figure 3
The distribution of residuals after the ANCOVA of
Exp. II is shown in Figure 3, and the inhomogeneity is clearly
discernible: there is a shallow oblique cloud of higher density on the
left side of the distribution. This cloud reflects the fact that as the
predicted RTtransp value becomes smaller and smaller (moving left along
the x-axis), the residuals tend to cluster at higher and higher values
(up along the y-axis). In other words, as the predicted values become
smaller, the errors, or discrepancies between the predicted values and
the observed ones, become systematically positive. This is a clear
indication of a floor effect, which is reasonable to
expect given that response times cannot go below some lower limit due
to
processing and motor limitations (though what this lower limit is may
vary
between observers). Indeed, if we mark the points for which RTtransp
had
the lowest values (110-230 ms, bold dots in Figure 3), they lie below
an
oblique line which is roughly parallel to the dense cloud above it.
(The exact
orientation of the line drawn was chosen arbitrarily. We hypothesized
that
these very short RTtransp values were due to anticipatory responses or
other
response errors, and therefore excluded them from the analysis. This
raised
the total number of outliers in the analysis to 25, since points
outside
the two horizontal lines, i.e., for which the z-scores were below –3.5
or
above 3.5, were also considered as outliers.) To validate this
explanation of the floor effect further, we examined the distribution
of residuals for observer 06, who had long response time (see Figure 8
of the paper), and further
restricted the set to the four cardinal directions. The distribution of
the
residuals is shown in Figure 4: the variances are clearly homogeneously
distributed.
Figure 4
The inhomogeneity of the distribution of the
residuals in Figure 3 indicates that, even after removal of the
outliers, the results of the ANCOVA are not exact. When coming to test
small interaction effects, one therefore needs to be careful. A
possible strategy is to restrict the analysis to subsets of the data
for which there is no floor effect, as illustrated in Figure 4. This
was done by selecting an observer with long response times. For this
observer, the effect of manipulating alpha on Ln(RTtransp) was almost
perfectly linear, in contrast to other observers. We argued in the
paper that
the linear effect of alpha was in fact the "true" effect of alpha, and
that
deviations from linearity were due to a floor effect. Control
experiments in the "Experiment III’ part of the paper could confirm
this hypothesis. Here
we can show that within the set of data of Experiment II this linear
relationship
can be observed for each observer. We restricted the analysis to the 7
naive
observers and to the 3 values of alpha which were used for all these
observers.
When we further restrict the set of data to parameters which lead to
larger
RTtransp values (component speed below 1.1 deg/sec, horizontal
directions),
the effect of alpha is almost linear for each observer (Figure 5), and
the
average curve is linear (solid line in Figure 6; the second order
coefficient
of the best fitting quadratic function is close to zero). On the other
hand,
when restricting the set of data to parameters which lead to smaller
RTtransp
values (component speed above 1.1 deg/sec, oblique directions), the
second
order coefficient of the best fitting quadratic function is not
negligible
(dashed line in Figure 6). The inspection of residuals for the
high-RTtransp
set of data confirms the relationship between floor effect,
non-homogeneity
of variances and observed non-linearity of alpha: the residuals
presented
in Figure 7 are homogenously distributed.
A maybe more direct estimation of the link between floor effect, non-homogeneity of variances and non linearity was obtained by looking at the interactions between the effect of alpha and of the global direction of motion for the nine observers. We found that these two variables had independant effects on RTtransp, even though the graphs showed some degree of interaction, due to the floor effect (Hupé, J.M., & Rubin, N. (2002) The oblique plaid effect. In prep. See also ARVO 2001 demo).Figure 5
Figure 6
Figure 7
Observer | Ln(RTtransp) | RTtransp (sec) | (Alpha, Cardinal) | F Value | P Value | Bartlett X2 (df=1) | P value |
O8 | 7.79 | 2.41 | F(1, 212) | 0.1 | 0.8112 | 0.5 | 0.3899 |
O7 | 6.94 | 1.03 | F(1, 212) | 2.1 | 0.1515 | 0.7 | 0.4029 |
O2 | 7.56 | 1.92 | F(1, 1015) | 0.0 | 0.9301 | 0.8 | 0.3794 |
O6 | 7.57 | 1.94 | F(1, 1144) | 10.4 | 0.0013 | 20.0 | 0.0001 |
O5 | 6.49 | 0.66 | F(1, 1136) | 76.8 | 0.0000 | 43.0 | 0.0000 |
O3 | 6.45 | 0.63 | F(1, 1034) | 131.8 | 0.0000 | 93.3 | 0.0000 |
O9 | 6.75 | 0.85 | F(1, 212) | 77.3 | 0.0000 | 107.6 | 0.0000 |
O1 | 6.69 | 0.81 | F(1, 1012) | 144.6 | 0.0000 | 138.2 | 0.0000 |
O4 | 6.70 | 0.81 | F(1, 1145) | 122.1 | 0.0000 | 191.9 | 0.0000 |
Table I : Interactions between "alpha" and "global direction"
(cardinal versus oblique directions) for observers with short RTtransp
are due to
a floor effect. For each observer (left-most column), we measured
the average response time (colums 2-3) to cardinal directions for the
largest tested value of alpha (160 deg in grp1, 165 deg in grp2 and 150
deg in grp3). The next three columns display the results of the
“homogeneity of slopes model”
linear analysis (which compares whether the linear regression curves of
alpha
on ln(RTtransp) are parallel for cardinal and oblique directions), and
the
two rightmost columns indicate whether the variances were homogenous or
not. The table was sorted by the ascending order of Bartlett Chi
Square
values (the larger the value the more different the variances).
There
is a strong correlation betwen the significance levels of the Bartlett X2
and of those of the linear analysis, and observers for which both tests
gave non-significant results tend to have longer response times.