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Th`ese Marouan BOUALI - Sites personnels de TELECOM ParisTech

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42 3. Standard <strong>de</strong>striping techniques and application to MODIS<br />

Detector Terra Band 27 Terra Band 30 Terra Band 33<br />

– Mean value Std <strong>de</strong>viation Mean value Std <strong>de</strong>viation Mean value Std <strong>de</strong>viation<br />

d 1 12982 1043.6 16933 2441.9 23072 1660.9<br />

d 2 12982 1043.6 16933 2441.4 23072 1660.9<br />

d 3 12982 1043.7 16934 2442.5 23072 1661.1<br />

d 4 12981 1043.7 16934 2442.1 23072 1661.3<br />

d 5 12982 1043.9 16934 2442.1 23072 1661.6<br />

d 6 12982 1043.9 16934 2442.1 23072 1661.0<br />

d 7 12984 1044.1 16934 2442.0 23072 1661.0<br />

d 8 12981 1044.0 16934 2442.0 23072 1660.9<br />

d 9 12980 1044.0 16934 2442.0 23072 1660.9<br />

d 10 12980 1043.9 16934 2442.0 23072 1660.6<br />

Table 3.1 – Mean/standard <strong>de</strong>viation values (DN) of 10 <strong>de</strong>tectors for Terra<br />

MODIS bands 27, 30 and 33. The small statistical <strong>de</strong>viation between <strong>de</strong>tectors<br />

discredits the application of moment matching on MODIS data<br />

The moment matching technique only rectifies first/second or<strong>de</strong>r statistics and as such<br />

requires a careful selection of the reference signal. If a <strong>de</strong>tector with strong statistical<br />

<strong>de</strong>viations from others (a <strong>de</strong>tector responsible for random stripes for exemple) is used<br />

as a reference, moment matching can result in very poor <strong>de</strong>striping. Many strategies based<br />

on the analysis of inter-<strong>de</strong>tector response statistics can be used (see section 3.4). A<br />

common option is to rely on mean/standard <strong>de</strong>viation values computed over the entire<br />

scene. Altough the simplicity of its implementation makes it a popular technique, moment<br />

matching suffers from many limitations <strong>de</strong>scribed in [Horn and Woodham, 1979]. A major<br />

issue pointed out on MSS is the impact of non-linearities in photomultipliers responses,<br />

presumably abscent in more sophisticated imaging <strong>de</strong>vices. Mean/standard <strong>de</strong>viation values<br />

reported in tables 3.1, 3.2 and experiments conducted on both Terra and Aqua MODIS<br />

data, illustrate how moment matching only results in partial <strong>de</strong>striping (figure 3.3). In<strong>de</strong>ed,<br />

the gain/offset mo<strong>de</strong>l only modifies the affine response of the <strong>de</strong>tectors and fails to<br />

take into account non-linear effects, highly responsible for residual stripes. Local analysis<br />

of MODIS swaths reveals a <strong>de</strong>pen<strong>de</strong>ncy of <strong>de</strong>tectors linear response to the signal intensity.<br />

This can be verified experimentally by estimating gains/offsets from swaths covering<br />

different levels of radiances (oceans and clouds). Furthermore, first or<strong>de</strong>r statistics make<br />

the method very sensitive to the geophysical content of the images. In many cases, small<br />

clouds or other highly reflective targets, are only visible by a limited set of <strong>de</strong>tectors and<br />

the resulting statistical bias is not accounted for in the moment matching procedure.<br />

3.3 Histogram Matching<br />

The hypothesis of linear and stationnary response exploited by the moment matching<br />

method is too strong to provi<strong>de</strong> reliable results on MODIS data. Investigation of<br />

tables 3.1, 3.2 shows that on Terra/Aqua bands severely contaminated with stripes, <strong>de</strong>tectors<br />

have very similar mean/standard <strong>de</strong>viation values. The visual examination of su-

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