S. Lovejoy et al., Multifractals and resolution-independent remote sensing algorithms: the example of ocean colour, INT J REMOT, 22(7), 2001, pp. 1191-1234
We argue that geophysical and geographical fields are generally characteris
ed by wide range scaling implying systematic, strong (power law) resolution
dependencies when they are remotely sensed. The corresponding geometric st
ructures are fractal sets; the corresponding fields are multifractals. Math
ematically, multifractals are measures that are singular with respect to th
e standard Lebesgue measures; therefore, they are outside the scope of many
of the methods of classical geostatistics. Because the resolution of a mea
surement is generally (due to technical constraints) much larger than the i
nner scale of the variability/scaling; the observations will be fundamental
ly observer dependent; hence, standard remote sensing algorithms that do no
t explicitly take this dependence into account will depend on subjective re
solution-dependent parameters. We argue that, on the contrary, the resoluti
on dependence must be systematically removed so that scale-invariant algori
thms independent of the observer can be produced. We illustrate these ideas
in various ways with the help of eight-channel, 7 m resolution remote ocea
n colour data (from the MIES II sensor) over the St Lawrence estuary. First
, we show that the data is indeed multiscaling over nearly four orders of m
agnitude in scale, and we quantify this using universal multifractal parame
ters. With the help of conditional multifractal statistics, we then show ho
w to use multifractals in various practical ways such as for extrapolating
from one resolution to another or from one location to another, or to corre
cting biases introduced when studying extreme, rare phenomena. We also show
how the scaling interrelationship of surrogate and in situ data can be han
dled using vector multifractals and examine the resolution dependence of pr
inciple components in dual wavelength analyses. Finally, we indicate why th
e standard ocean colour algorithms have hidden resolution dependencies. and
we show how they can (at least in principle) be removed.