Abstract
Sand dune movement is a hazardous phenomenon in Egypt and creates major threat on the existing land use and land cover as well as developmental plans. This paper studied the sand dune morphology and quantified the rate of sand dune movements and direction in a newly developed project in the southwest of Egypt. Two dates of satellite imageries were used to trace the Barchan dunes at various sites with different morphological properties to estimate the annual movement rate based on point to point geo-correlations. 149 dunes of the common sand dunes in the area of study including barchans and transverse dunes were studied to accurately determine their rate of movements, which ranged from 1.3 to 19.3 my-1. The direction of sand dune movements was mainly to the south and slightly southeast with range from 265 to 295 degrees. The quantification of sand dune movement and direction has, indeed, enabled to determine the major threat on the exiting land use and land cover as well as the newly developmental projects.
Highlights
Egypt population is ~90 million, which, settles on just 6.6% of the Egyptian territory along the flood plain of the Nile Delta and the River Nile [1]
The main issue was the availability of water and suitability of land [2,3]; critical missed issue was the risk of the natural hazards of sand dune movements
South western desert of Egypt is occupied by a very complicated wind system, which is characterized by multidirections and intensities
Summary
Egypt population is ~90 million, which, settles on just 6.6% of the Egyptian territory along the flood plain of the Nile Delta and the River Nile [1]. The over increase of population has inspired both government and individuals for lateral spread towards the desert land. One of the main targeted areas for lateral expansion is the western desert but at specific localities such as the western corner of the western desert. In this area, the government initiated huge developmental projects including agriculture, urban and medical tourism. Various prominent projects have been developed in this area including land reclamation for agricultural purposes such as Toshka Project. The main issue was the availability of water and suitability of land [2,3]; critical missed issue was the risk of the natural hazards of sand dune movements. The success of such promising projects basically relies on understanding the dynamic of geomorphic landscapes that host these projects [4,5,6,7]
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