Impact of climate change on groundwater recharge in a small catchment in the Black Forest, Germany

• Published in: Hydrogeology journal 2012-05, Vol.20 (3), p.547-560
• Main Authors: Neukum, Christoph, Azzam, Rafig
• Format: Article
• Language: English
• Subjects: Air temperature; Aquatic Pollution; Catchment areas; Catchments; Climate change; Discharge; Drought; Earth and Environmental Science; Earth Sciences; Environmental impact; Forests; Freshwater; Geology; Geophysics/Geodesy; Groundwater; Groundwater data; Groundwater recharge; Hydrogeology; Hydrologic cycle; Hydrologic data; Hydrology/Water Resources; Rain; River discharge; River flow; Rivers; Runoff; Surface runoff; Surface water; Surface-groundwater relations; Temporal logic; Valleys; Waste Water Technology; Water exchange; Water Management; Water Pollution Control; Water Quality/Water Pollution
• ISSN: 1431-2174; 1435-0157
• DOI: 10.1007/s10040-011-0827-x

Temporal and spatial changes of the hydrological cycle are the consequences of climate variations. In addition to changes in surface runoff with possible floods and droughts, climate variations may affect groundwater through alteration of groundwater recharge with consequences for future water management. This study investigates the impact of climate change, according to the Special Report on Emission Scenarios (SRES) A1B, A2 and B1, on groundwater recharge in the catchment area of a fissured aquifer in the Black Forest, Germany, which has sparse groundwater data. The study uses a water-balance model considering a conceptual approach for groundwater-surface water exchange. River discharge data are used for model calibration and validation. The results show temporal and spatial changes in groundwater recharge. Groundwater recharge is progressively reduced for summer during the twenty-first century. The annual sum of groundwater recharge is affected negatively for scenarios A1B and A2. On average, groundwater recharge during the twenty-first century is reduced mainly for the lower parts of the valley and increased for the upper parts of the valley and the crests. The reduced storage of water as snow during winter due to projected higher air temperatures causes an important relative increase in rainfall and, therefore, higher groundwater recharge and river discharge.