Abstract

The aim of this study is to assess the land use/land cover (LULC) inter-seasonal changes along the Cameroonian shores of Lake Chad and its hinterland using the four generations of Landsat sensors images of MSS, TM, ETM+ and OLI. Identification of land use/land cover inter-seasonal changes is based on classification by Support Vector Machines (SVMs) algorithm. Three major spatial classes of objects are identified: open water, vegetation and marshlands, and bare soils. The results show that, bare soils class has the higher rate, and can reach 67.57% of the study area extent. Moreover, land use/land cover change from one season to another or from one decade to another can be closely linked to evolution of climate conditions. Then open water areas vary little with rate of 1.94% and 7.6% for inter-seasonal changes, and rate of 5.62% and 63.05% for inter-annual changes. Compared to open water, vegetation and marshlands has the most important variation, that is 583.59%. In addition, proportions of bare soils that vary are different between dry seasons and rainy seasons, with a lower and a higher rate of 5.38% and 82.8%. This leads to the conclusion that occupation in the study area is dominated by bare soils principally; occupation class that is most affected by changes is vegetation and marshlands followed by bare soils and then open water and marshlands.

Highlights

  • Land use/land cover (LULC) changes play a major role in the study of environment change (Reis, 2008), (Vitousek, 1992)

  • Except in March 1973, vegetation, occupies more than one quarter of LULC during the rainy season and the dry season, with areas extent between 120519,6 Ha to 356612,3 Ha, which corresponds to percentages between 25.38% to 75.09%

  • Monitoring land use/land cover to detect development trends is, highly useful in this context and remote sensing technology have played an important role in this analysis

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Summary

Introduction

Land use/land cover (LULC) changes play a major role in the study of environment change (Reis, 2008), (Vitousek, 1992). Despite the physiognomic analysis of the lake by scientists, using hydrological data, field observation and satellite imagery (Rangé, 2016), (Olivry, 1996), (Magrin 2015), (Geerken, Vassolo, and Bila, 2010), some interpretations of evolution of the lake Chad land cover are still inaccurate (Lemoalle, 2014). This is the case of marshland flooded, which are difficult to identify on satellite imagery and not sufficiently taken into account when estimating the lake surface (Rangé, 2016). Concerning « Little Chad » (Tilho, 1928), (Olivry 1996), (Magrin 2015), draws schematic map of lake Chad’s average situation around 2010, on which it can be observed that Cameroonian side is occupied by permanent open water, almost permanent marshland, marshland that is irregularly flooded and areas not flooded since 1963

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