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Bootstrapping therefore represents a powerful and simple tool for accept-
ing or rejecting our fi rst estimate of the correlation coeffi cient. The applica-
tion of the above procedure applied to the synthetic sediment data yields a
clear unimodal gaussian distribution of the correlation coeffi cients.
corrcoef(meters,age)
ans =
1.0000 0.9342
0.9342 1.0000
rhos1000 = bootstrp(1000,'corrcoef',meters,age);
hist(rhos1000(:,2),30)
Most rhos1000 fall within the interval between 0.88 and 0.98. Since the
resampled correlation coeffi cients obviously are gaussian distributed, we
can use the mean as a good estimate for the true correlation coeffi cient.
mean(rhos1000(:,2))
ans =
0.9315
This value is not much different to our fi rst result of r =0.9342. However,
now we can be certain about the validity of this result. However, in our
example, the bootstrap estimate of the correlations from the age-depth data
is quite skewed, as there is a hard upper limit of one. Nevertheless, the boot-
strap method is a valuable tool for obtaining valuable information on the
reliability of Pearson·s correlation coeffi cient of bivariate data sets.
4.3 Classical Linear Regression Analysis and Prediction
Linear regression provides another way of describing the dependence be-
tween the two variables x and y . Whereas Pearson·s correlation coeffi cient
only provides a rough measure of a linear trend, linear models obtained by
regression analysis allow to predict arbitrary y values for any given value
of x within the data range. Statistical testing of the signifi cance of the linear
model provides some insights into the quality of prediction.
Classical regression assumes that y responds to x, and the entire disper-
sion in the data set is in the y -value (Fig. 4.4). Then, x is the independent
or regressor or predictor variable. The values of x is defi ned by the experi-
mentalist and are often regarded as to be free of errors. An example is the
location x of a sample in a sediment core. The dependent variable y contains
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