Impact du changement de climat sur la recharge en eau souterraine d’un petit bassin versant de la Forêt Noire, Allemagne Einfluss des Klimawandels auf die Grundwasserneubildung in einem kleinen Einzugsgebiet im Schwarzwald, Deutschland Impacto del cambio climático sobre la recarga del agua subterránea en una pequeña cuenca hidrográfica en la Selva Negra, Alemania 气候变化对德国黑森林区小流域地下水补给的影响 Impacte das alterações climáticas na recarga de água subterrânea numa pequena bacia da Floresta Negra, Alemanha

Neukum, Christoph; Azzam, R.

Impact du changement de climat sur la recharge en eau souterraine d’un petit bassin versant de la Forêt Noire, Allemagne Einfluss des Klimawandels auf die Grundwasserneubildung in einem kleinen Einzugsgebiet im Schwarzwald, Deutschland Impacto del cambio climático sobre la recarga del agua subterránea en una pequeña cuenca hidrográfica en la Selva Negra, Alemania 气候变化对德国黑森林区小流域地下水补给的影响 Impacte das alterações climáticas na recarga de água subterrânea numa pequena bacia da Floresta Negra, Alemanha | Impact of climate change on groundwater recharge in a small catchment in the Black Forest, Germany

2012

Neukum, Christoph | Azzam, R. (Rafig)

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.

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