CHAPTER ONE
INTRODUCTION
1.1 BACKGROUND OF STUDY
Water is indispensable for life, but its availability at a sustainable quality and quantity is threatened by many factors, of which climate plays a leading role (IPCC, 1995). Groundwater is the major source of drinking water in Africa and has a rapidly expanding role in irrigation to combat growing food insecurity. This module deals with both the impact of climate change on groundwater resources, It is important to recall the global extent of climate change, and to consider the impacts on the scale of the global hydro logic cycle. Of Africa’s population of 1 billion, roughly 60% live in rural areas. Around 80% of them rely on ground water based community or household supplies for domestic and other water needs (WHO/UNICEF, 2008). Currently there are more than 300 million people in Africa without access to safe drinking water, many of whom are amongst the poorest and most vulnerable in the world (MacDonald, A.; Bonsor, H.C.; Dochartaigh, B.E.O.;
Taylor, R.,, 2012). Climate variability and change influences groundwater systems both directly through replenishment by recharge and indirectly through changes in groundwater use. These impacts can be modified by human activity such as land-use change (Taylor, Nature Climate change, 2013). Climate change is “an altered state of the climate that can be identified by change in the mean and/or variability of its properties and that persists for an extended period, typically decades or longer”. It may be due to “natural internal processes or external forcing, or to persistent anthropogenic changes in the composition of the atmosphere or in land use” (IPCC, 2007). Climate change affects water resources around the world in generally unknown ways. Potential impacts of climate change on surface water particularly projected regional climate patterns and trends (i.e., climate variability and change) have been studied in some detail.
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