5 research outputs found

    Intégration des données spectrales et géomorphométriques pour la caractérisation de la dégradation des sols et l'identification des zones desusceptibilité à l'érosion hydrique

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    In the field of spatial observations of arid and semiarid ecosystems, the interest of remote sensing has long been recognised. The present work investigates the use of remote sensing techniques and digital elevation model analysis to characterise land degradation processes. The main objective is to evaluate the potential of spectral data and geomorphometric variables to discriminate different levels of soil degradation, and to assess ecosystems fragility and their susceptibility to degradation and desertification phenomena. The methodology adopted uses an integrated approach that combines spectral measurements, provided by remote sensing images, and geomorphometric variables, derived from a digital elevation model, in an attempt to define a set of indicators (spectral and topographic) of geomorphic processes and land degradation. Remote sensing techniques are based on two approaches: spectral mixture analysis that deals with heterogeneity at the sub-pixel level, and a set of indices describing the spectrum shape, which are sensitive to soil surface conditions. Integration procedures were involved in two ways. The first is in the correction of terrain-induced image distortions, which provide images free from relief displacement effects (ortho-rectification), and in the removal of topographically induced effects on TM images through a combined atmospheric and topographic correction. The second is in a parametric integration of spectral data and geomorphometric attributes to assess land susceptibility to degradation and desertification processes. Two types of data were collected for this research: satellite optical imagery and ground-based spectro-radiometric measurements. While indices describing soil colour (corresponding to colour parameters Intensity, Hue and Saturation) were used to discriminate different levels of soil degradation based on both ground and satellite data, the spectral mixture analysis was performed on the image to derive relative abundance of scene components. The results show that the spectral indices have enough potential to discriminate different levels of degradation, particularly when bands from the short-wave infrared domain are included (TM5 and TM7). They demonstrate results similar to those generated by spectral unmixing for the assessment of land degradation features in general, and soil erosion in particular. Concerning terrain analysis, this study points up the interest of the integrated use of local topographic attributes and combined topographic indices to characterise the hydrologic behaviour of terrain units, and to understand its effects on landscape evolution. These topographic variables quantify the contextual nature of points and characterise the spatial variability of processes occurring in the landscape. They are the major factors controlling the direction and the intensity of hillslope and hydrologic processes. The latter are responsible for the landscape evolution and its exposure to degradation risks by water erosion. Compared to the method based on curvatures analysis, our approach allows a better identification of homogeneous response units to hydrologic processes. These units are in agreement with flow directions and with the principles governing water and substance motion on the hillslope. Finally, we carried out an integrated analysis of geo-ecological parameters describing the studied ecosystem. It consists in defining hydrologic response units through an integration of spectral information and geomorphometric attributes. This allows us to determine the ecosystem fragility and to evaluate its susceptibility to land degradation and desertification processes

    : Mapping dominant woody species distribution in the Middle Atlas mountains (Morocco) from ASTER imagery.

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    International audienceThe cedar forest of the Middle Atlas of Morocco is characterized by the heterogeneity of its stands and its fragmentation caused by the interaction between various factors such as human activities, soil variability and climatic fluctuations. This results in a spatial and spectral heterogeneity that limits the reliability of the conventional methods used for classification of satellite imagery. To address this issue, the present study uses methods based on spectral similarity to map major forest species of the cedar forest of Morocco: Linear spectral mixture analysis (LSMA) andSpectral angle mapper (SAM). The aim of the study was to compare: (i) methods used to extract spectral signatures of pure pixels (endmembers) from the imagery, and (ii) the performances of LSMA and SAM in terms of appropriately mapping major forest species of the Middle Atlas. To achieve these goals, we used ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) images for the forest mapping. The results showed that SMA and SAM have led to similar patterns of the spatial distribution of the studied forest species, but these generated noticeable differences in the areas assigned to each mapped class. The classification results obtained by SMA and SAM werecompared to those generated by the maximum likelihood classification method (our reference). This procedure showed that SMA yielded a better classification of the dominant forest species than SAM; this is illustrated by the value of Kappa Coefficient which was about 0.70 for the SMA method and 0.66 for the SAM approach.La cĂ©draie du Moyen Atlas, au Maroc, est caractĂ©risĂ©e par l’hĂ©tĂ©rogĂ©nĂ©itĂ© de ses peuplements ainsi que par la fragmentation de son espace forestier. Ces caractĂ©ristiques rĂ©sultent de l’interaction de divers facteurs anthropiques, pĂ©dologiques et climatiques. Ces hĂ©tĂ©rogĂ©nĂ©itĂ©s spatiale et spectrale limitent la fiabilitĂ© des mĂ©thodes conventionnelles de classification de l’imagerie satellitaire. Dans la prĂ©sente Ă©tude, on suggĂšre d’utiliser les mĂ©thodes basĂ©es sur la similaritĂ© spectrale pour cartographier les espĂšces forestiĂšres dominantes de l’écosystĂšme de la cĂ©draie, soit l’analyse de mixture spectrale linĂ©aire (AMSL) et le Spectral angle mapper (SAM). Les objectifs poursuivis consistent Ă  comparer des procĂ©dures d’extraction des signatures spectrales « pures » prototypes, dites endmembers, et les approches de l’AMSL et du SAM en termes de cartographie des espĂšces vĂ©gĂ©tales dominantes de cette forĂȘt. Pour atteindre ces objectifs, on a utilisĂ© des images acquises par le capteur ASTER (Advanced spaceborne thermal emission and reflection radiometer). Les rĂ©sultats obtenus montrent que l’utilisation des mĂ©thodes de l’AMSL et du SAM a abouti Ă  des rĂ©sultats similaires en termes de rĂ©partition des espĂšces cartographiĂ©es, mais avec des diffĂ©rences au plan des superficies occupĂ©es par ces espĂšces. La comparaison des rĂ©sultats obtenus Ă  l’aide de l’AMSL et du SAM avec ceux de la classification par maximum de vraisemblance (notre rĂ©fĂ©rence) dĂ©montre que l’AMSL a permis de classifier les espĂšces forestiĂšres dominantes avec une meilleure prĂ©cision que le SAM, ce qui s’exprime par un coefficient Kappa de l’ordre de 0,7 pour la mĂ©thode de l’AMSL contre 0,66 pour l’approche du SAM
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