Journal Article
Quantifying the modern recharge of the “fossil” Sahara aquifers
Goncalves, J., Petersen, J., Deschamps, Hamelin, P.B. and Baba-Sy, O.
Record Number:
3985
Year:
2013
Journal:
Geophysical Research Letters
Pages:
2673–2678
Volume:
40
Abstract:
The North-Western Sahara Aquifer System (NWSAS), one of the world’s largest groundwater systems, shows an overall piezometric decline associated with increasing
withdrawals. Estimating the recharge rate in such a semiarid system is challenging but crucial for sustainable water development. In this paper, the recharge of the NWSAS is estimated using a regional water budget based on GRACE terrestrial water storage monthly records, soil moisture from the GLDAS (a land data system that
assimilates hydrological information), and groundwater pumping rates. A cumulated natural recharge rate of 1.40 ˙ 0.90 km3 yr–1 is estimated for the two main aquifers.
Our results suggest a renewal rate of about 40% which partly contradicts the premise that recharge in this area should be very low or even null. Aquifer depletion inferred from
our analysis is consistent with observed piezometric head decline in the two main aquifers in the region. Annual recharge variations were also estimated and vary between
0 and 4.40 km3 yr–1 for the period 2003–2010. These values correspond to a recharge between 0 and 6.75 mm yr–1 on the 650,000 km2 of outcropping areas of the aquifers,
which is consistent with the expected weak and sporadic recharge in this semiarid environment. These variations are also in line with annual rainfall variation with a lag time of about 1 year. Citation: Gonçalvès, J., J. Petersen, P. Deschamps,
B. Hamelin, and O. Baba-Sy (2013), Quantifying the modern recharge of the “fossil” Sahara aquifers, Geophys. Res. Lett., 40, 2673–2678, doi:10.1002/grl.50478.
Times Cited:
0