Evaluation By Remote Sensing Of The Withdrawn Water Volume From The Aquifer System Of The Spatientrional Sahara

The present report shows the contribution of remote sensing to estimate the volume of water withdrawn from aquifers for a semi-arid or arid climate such as that in our study area the Aquifer System of Spatientrional Sahara. The vegetation area was firstly estimated from a spatial distribution of vegetation indices from the MOD13Q1 product of the MODIS sensor for a period from 2001 to 2011 by an algorithm highlighting the pixels in the red and the infrared. Its on average almost constant at 500 km2 for all the years. Furthermore evapotranspiration was defined spatially and statistically by the MOD16A2 product on the whole basin for 2011. The statistics are derived from an algorithm ensuring the logic based on the Penman-Monteith equation. These statistics regarding the area of vegetation gave the annual total volume of withdrawn water because this volume is evaporated in the absence of rainfall in the water balance and the depth of the basin does not allow it to vary in the grounds level. There was extraction more than 25 billion meters-cube. This means that the enormity of the consumption that is indeed a few hundred m3s. It presents a serious risk of salinity and flow reversal towards the sea. Such a calculation is developed depending on remote sensing elements such as the spatial and temporal resolutions.