Abstract:
Climate change poses uncertainties to the supply and management of water resources. The
Intergovernmental Panel on Climate Change (IPCC) estimates that the global mean surface temperature has
increased 0.6 ± 0.2 oC since 1861, and predicts an increase of 2 to 4 oC over the next 100 years. Temperature
increases also affect the hydrologic cycle by directly increasing evaporation of available surface water and
vegetation transpiration. Consequently, these changes can influence precipitation amounts, timings and
intensity rates, and indirectly impact the flux and storage of water in surface and subsurface reservoirs (i.e.,
lakes, soil moisture, groundwater). In addition, there may be other associated impacts, such as sea water
intrusion, water quality deterioration, potable water shortage, etc. While climate change affects surface water
resources directly through changes in the major long-term climate variables such as air temperature,
precipitation, and evapotranspiration, the relationship between the changing climate variables and
groundwater is more complicated and poorly understood. The greater variability in rainfall could mean more
frequent and prolonged periods of high or low groundwater levels, and saline intrusion in coastal aquifers due
to sea level rise and resource reduction. Groundwater resources are related to climate change through the
direct interaction with surface water resources, such as lakes and rivers, and indirectly through the recharge
process. The direct effect of climate change on groundwater resources depends upon the change in the volume
and distribution of groundwater recharge. Therefore, quantifying the impact of climate change on groundwater
resources requires not only reliable forecasting of changes in the major climatic variables, but also accurate
estimation of groundwater recharge. A number of Global Climate Models (GCM) are available for
understanding climate and projecting climate change. There is a need to downscale GCM on a basin scale and
couple them with relevant hydrological models considering all components of the hydrological cycle. Output of
these coupled models such as quantification of the groundwater recharge will help in taking appropriate
adaptation strategies due to the impact of climate change. This article presents the likely impact of climate
change on groundwater resources, climate change scenario for groundwater in India, status of research studies
carried out at national and international level, and methodology to assess the impact of climate change on
groundwater resources.