Quantification of the functional relation between remotely-sensed data
and commensurable ground based observations is a basic prerequisite i
n many remote sensing studies. To this end, linear regression analysis
is generally employed. Given two matrices of paired noise-infected me
asurements, classical linear regression is usually employed to find op
timal parameters of a model calibration function which fits the observ
ed readings best, in the minimal least squares sense. The squared coef
ficient of determination R=(variation due to the model)/(total variati
on) is a common quality measure of the chosen model, while the varianc
e S-r of the 'residuals' is a measure of the information that the chos
en calibration function is unable to explain. The basic premise of reg
ression analysis requires that the reference ground data must be preci
se and noiseless. Since in most remote sensing studies this condition
is not met, classical regression is not an efficient tool for discover
ing the true functional relation between remotely-sensed data and grou
nd observations. A new calibration method is proposed whereby the leas
t-squares minimization is conducted on the amplitude matrices of the r
eadings via the FFT. For a given model, R is always increased beyond t
he value obtained by conventional regression at the expense of a sligh
t increase in S-r. When one of the measurement sets may be considered
noiseless, phase correction may be employed to reduce S-r as well, bel
ow the value obtained by conventional regression. The new calibration
method is a radical departure from classical statistics and has the po
tential of significantly improving statistical inference in remote sen
sing. The line taken is illustrated by numerical examples which compar
e the new calibration method to the classical regression technique. It
is demonstrated, that the new method can discover better the true fun
ctional relation between satellite images or between ground based sens
or arrays and satellite images, which may be occluded by noise.