Impacts of Climate Change and of Anthropisation on Water Resources: from the Risk Assessment to Adaptation, the Case of the Seine Basin (including Paris, France)

Wednesday, 16 December 2015: 12:00
3020 (Moscone West)
Florence Habets1,2, Pascal Viennot3, Charlotte Thierion4, Jean-Pierre Vergnes2, Ahmed Ait Kaci5 and Yvan Caballero6, (1)CNRS, Paris Cedex 16, France, (2)University Pierre and Marie Curie Paris VI, Paris, France, (3)Mines ParisTech, Geosciences Center, Fontainebleau, France, (4)Antea Group, Olivet, France, (5)BIPE, Issy les Moulineaux, France, (6)BRGM, Orléans, France
The Seine river, located in the temperate climate of northern France and flowing over a large sedimentary basins that hosts multilayer aquifers, is characterized by small temporal variations of its discharge. However, the presence of a megacity (Paris) and a wide area of intensive agriculture combined with climate change puts pressure on the water resources both in terms of quality and quantity.

Previous research projects have estimated the impact of climate change on the water resource of the Seine basin, with the uncertainties associated to climate projections, hydrological models or downscaling methods. The water resource was projected to decrease by -14 % ± 10 % in 2050 and -28 +/-16% in 2100. This led to new studies that focus on the combined impact of climate change and adaptations. The tested adaptations are: a reduction of the groundwater abstractions, evolution of land use, development of small dams to « harvest water » or artificial recharge of aquifers.

The communication of the results of these projects to stakeholders have led to the development on new indicators that better express the risk on the water resource management, especially for the groundwater. For instance maps of the evolution of piezometric head are difficult to interpret. To better express the risk evolution, a new indicator was defined: the evolution of the groundwater crisis duration, ie, the period when the charge of the aquifer is below the crisis piezometric level defined by the stakeholders. Such crisis piezometric levels are used to help defining the period when the groundwater abstraction should be reduced. Such maps are more efficient to communicate with water resources managers.

This communication will focus on the results from the MEDDE Explore 2070 and ANR Oracle projects.