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Th`ese Marouan BOUALI - Sites personnels de TELECOM ParisTech

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12 1. Introduction<br />

A common issue for Earth observing instruments, known as striping effect have persisted<br />

for more then 30 years, i.e, since the launch of Landsat 1. It was since reported on<br />

many imaging spectrometers :<br />

- Landsat Multi Spectral Scanner (MSS) and Thematic Mapper (TM)<br />

- Geostationary Operational Environmental Satellites (GOES)<br />

- Advanced Very High Resolution Radiometer (AVHRR)<br />

- Mo<strong>de</strong>rate Resolution Imaging Spectrometer (MODIS)<br />

- Compact High Resolution Imaging Spectrometer (CHRIS)<br />

- HYPERION<br />

- MEdium Resolution Imaging Spectrometer (MERIS)<br />

- Compact Reconnaissance Imaging Spectrometer for Mars (CRISM)<br />

- GLobal Imager (GLI)<br />

- Advanced Land Imager (ALI)<br />

The previous list inlu<strong>de</strong>s both whiskbroom and pushbroom sensors which are the two<br />

main techniques used for Earth observation.<br />

Whiskbroom instruments, also known as cross-track scanners acquire a series of lines in<br />

the direction perpendicular to the satellite orbital motion. A scan sweep from one si<strong>de</strong> of<br />

the swath to the other is ensured by a continuously rotating mirror. A limited set of <strong>de</strong>tectors,<br />

sensitive to spectific wavelenghts, then captures the radiation emitted or reflected<br />

by the Earth before its convertion into digital numbers.<br />

Pushbroom sensors (along-track scanners) also exploit the orbital motion of the platform<br />

to generate the second dimension of the acquired signal. They differ from the whiskbroom<br />

<strong>de</strong>sign in that the rotating mirror is replaced by a linear array of numerous <strong>de</strong>tectors that<br />

capture simultaneously each pixel of a single scan line.<br />

In both acquisition principles, images are formed by enterlacing or concatanating scan<br />

lines, acquired separately by different <strong>de</strong>tectors. Consequently, the imperfect calibration<br />

of individual <strong>de</strong>tectors induces a sharp pattern across or along the scanning direction that<br />

compromises both visual interpretation and quantitative analysis. More specifically, striping<br />

is disturbingly visible over low-radiance homogeneous regions, which often coinci<strong>de</strong><br />

with oceanographic areas. In fact, the impact of stripe noise on satellite <strong>de</strong>rived geophysical<br />

variables, including ocean color products, is increasingly attracting the interest of<br />

remote sensing research groups.<br />

Although an extensive litterature has tackled the striping issue, existing techniques are<br />

often not able to satisfie the requirements imposed by several remote sensing applications<br />

namely, complete stripe removal without signal distortion or additional post-processing<br />

artifacts.<br />

The goal of this thesis is to analyse the limitations of standard <strong>de</strong>striping methods<br />

and to explore the issue of stripe noise removal using variational mo<strong>de</strong>ls. We illustrate the

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