The Etablissement Public Territorial de Bassin Somme (the regional public body of the Somme catchment area - AMEVA) has commissioned BRGM to carry out a study to anticipate possible future stresses on the water resources of the Somme catchment area (the Craie aquifer and the network of watercourses that drains it) in the context of climate change, and to assess the impacts of several prospective adaptation scenarios.
9 October 2024
Deviation in mean monthly piezometric levels (m) for three periods (short, medium and long term) compared with the 1981-2010 reference period (top: projection contrasted with a hot, dry climate; and bottom: median projection with limited changes in climate) - RCP85.

Deviation in mean monthly piezometric levels (m) for three periods (short, medium and long term) compared with the 1981-2010 reference period (top: projection contrasted with a hot, dry climate; and bottom: median projection with limited changes in climate) - RCP85.

© BRGM

The need

Climate change has an impact on the water cycle and water reserves. Due to the pressures exerted and the hydrogeological context, the surface water and groundwater resources of the Somme catchment area appear to be particularly vulnerable to climate change, the quantitative impacts of which are estimated using the hydrogeological model of the Somme developed by BRGM since 2000.

The results

The climate forcing factors were selected from the DRIAS portal, which provides climate projections by region in various graphical or numerical forms, produced by French climate modelling laboratories (IPSL, CERFACS, CNRM). Given the uncertainties of the climate models with regard to rainfall, a narrative approach has been adopted that considers two contrasting projections (a hot, dry climate and a median climate with limited changes).

The general trend in mean piezometric anomalies and mean flows suggests that in the short term (up to 2040) it will be slightly wetter, while the medium term (2041-2070) shows dry anomalies that become more pronounced or, on the contrary, invert in the long term (2071-2100) depending on the projection: the contrasted projection shows marked dry anomalies over the whole catchment area, while the median projection shows wet anomalies.

Projecting current abstraction rates into future scenarios shows that they exacerbate low water levels and droughts. The resource is highly stressed in some of the management units of the catchment area, intensifying conflicts between different uses (irrigation, drinking water supply and industry) in the context of climate change.

With regard to extreme events (hydrogeological low and high water), low/high water and low/maximum flow episodes become more frequent, longer and more intense from the medium term onwards than over the current period. In other words, current extremes will be normal in the future.

Finally, the implementation of abstraction reduction scenarios (National Water Plan) has shown that it is possible to maintain water resources in their current state in the near future. However, further reductions will be necessary from 2040 and beyond to conserve the water system.

Illustration of the trend in triggering drought threshold alerts in the Avre management unit at Moreuil (80) in a median climate projection.

Illustration of the trend in triggering drought threshold alerts in the Avre management unit at Moreuil (80) in a median climate projection.

 © BRGM

Using the results

The trends expressed in the results of this study will provide local stakeholders with specific information on which to base their water resource management decisions. The results obtained also help to estimate the volumes that can be abstracted from the catchment area.

The partners

  • Etablissement Public Territorial de Bassin Somme (regional public body of the Somme catchment area - AMEVA)
  • SAGE Haute Somme, SAGE Somme downstream and coastal watercourses
  • Artois-Picardy Water Agency
  • FEDER