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Extra info for Climate Change Effects on Groundwater Resources
From the 1970s through the 1990s, the Sahel experienced a drought relative to 1925–2000 averages (Nicholson and Grist 2001; Le Barbé et al. 2002). The geology of southern Mali consists predominantly of two rock types: the majority of the principal study region lies within the Birimian Precambrian weathered basement rock (largely comprised of metamorphosed sedimentary or igneous rocks). Lower Cambrian or Palaeozoic sedimentary rocks forming a “Sandstone Plateau” are present along the northern and eastern periphery of the Birimian (United Nations 1988; ARP Développement 2003).
Florke, M. (2005) Global-scale estimation of diffuse groundwater recharge. Frankfurt Hydrology Paper 03. Frankfurt am Main, Germany, Institute of Physical Geography, University of Frankfurt. C. R. (2007) A single layer soil water balance model or estimating deep drainage (potential recharge): An application to cropped land in semi-arid North-east Nigeria. Geoderma, 140, 119–131. , Diekkrüger, B. & Steup, G. (2006a) Physically modelling of hydrological processes in a tropical headwater catchment in Benin (West Africa) – process representation and multi-criteria validation.
P. J. (2008) Atmospheric warming and the amplification of precipitation extremes. Science, 321, 1481–1484. R. J. (2002) Constraints on future changes in climate and the hydrologic cycle. Nature, 419, 224–232. , Muttiah, R. R. (1998) Large area hydrologic modelling and assessment, Part 1 model development. Journal of the American Water Resources Association, 34, 73–89. Bradley, B. (2011) A synthesis of geological history and assessment of the hydrogeology of the Katonga Valley in southwest Uganda with evidence from apatite fission track analysis and electrical resistivity tomography.