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

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 manag...

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Bibliographic Details
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
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Summary: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.
ISSN:1431-2174
1435-0157
DOI:10.1007/s10040-011-0827-x