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Water at the heart of global geopolitical issues

What future can we expect for water resources in France?

Eric Sauquet, Research Director in Hydrology at INRAE
On October 23rd, 2024 |
4 min reading time
Eric Sauquet
Eric Sauquet
Research Director in Hydrology at INRAE
Key takeaways
  • The recent Explore2 project examines possible future scenarios regarding water in mainland France, based on the IPCC’s climate scenarios.
  • In the worst-case scenario, temperatures will increase by 4°C by the end of the century when compared to temperatures in 1976-2005, with increased precipitation in winter and reduced precipitation in summer.
  • A large part of mainland France will almost certainly experience more severe low-water levels in summer and higher river flows in winter.
  • The “hot spots” (notably the south-east and south-west of France) will be particularly affected by a drop in annual water resources.
  • Geographically, France is at the transition point between two major changes: more precipitation in northern Europe and aridification in the Mediterranean basin.

Cli­mate change is affect­ing the water cycle. As we have explored in this dossier, although water is abun­dant on Earth, it is uneven­ly dis­trib­uted in terms of both time and space, and ten­sions over the resource are increas­ing as a result of uses and cli­mate change. What is the sit­u­a­tion in France? The Explore21 project – the results of which were pub­lished in sum­mer 2024 – explores the pos­si­ble future of water in main­land France accord­ing to the cli­mate sce­nar­ios of the Inter­gov­ern­men­tal Pan­el on Cli­mate Change (IPCC). For var­i­ous water resource indi­ca­tors (riv­er flow, ground­wa­ter recharge, etc.), future lev­els are esti­mat­ed every 8 kilo­me­tres. Éric Sauquet, the project’s sci­en­tif­ic co-leader, explains the results.

How is climate change affecting the climate in mainland France?

Éric Sauquet. What­ev­er our future green­house gas (GHG) emis­sions, the tem­per­a­ture will rise, and the more emis­sions we pro­duce, the high­er the tem­per­a­ture. In the Explore2 study, we con­sid­ered three sce­nar­ios for future GHG emis­sions. I’m going to focus on the worst-case sce­nario, in which our GHG emis­sions con­tin­ue to grow sig­nif­i­cant­ly (RCP 8.5). In main­land France, the mod­els show that the tem­per­a­ture will be 4°C high­er by the end of the cen­tu­ry than it was between 1976 and 2005. The sit­u­a­tion will vary from sea­son to sea­son, with high­er tem­per­a­ture ris­es in sum­mer than in win­ter. As for pre­cip­i­ta­tion, it is like­ly to increase in win­ter and decrease in sum­mer by 2100. The sig­nal is not clear on an annu­al scale.

Pro­ject­ed changes in mean annu­al tem­per­a­ture for four con­trast­ing futures (Explore2 nar­ra­tives) under a sce­nario of high emis­sions at the end of the cen­tu­ry (ref­er­ence: 1976–2005).

What are the consequences for water resources?

Changes in riv­er flow reflect changes in rain­fall. It is almost cer­tain that a large part of main­land France will expe­ri­ence more severe low-water peri­ods in sum­mer, as a result of reduced rain­fall and increased evap­o­tran­spi­ra­tion. In win­ter, riv­er flow will increase over a large part of the coun­try due to the rise in pre­cip­i­ta­tion. With ris­ing tem­per­a­tures, rain­fall in the moun­tains will increase at the expense of snow­fall: this will con­tribute to high­er win­ter flows in the Alps, the Pyre­nees and the Mas­sif Cen­tral. On an annu­al scale, there is no clear trend in flows, with the excep­tion of the south of France, where the mod­els clear­ly show a reduc­tion in annu­al flows.

Pro­ject­ed changes in mean win­ter dis­charge for four con­trast­ing futures (Explore2 nar­ra­tives) under a sce­nario of high end-of-cen­tu­ry emis­sions (ref­er­ence: 1976–2005) (medi­an esti­mate for all hydro­log­i­cal mod­els combined)

In win­ter, riv­er flow will increase over a large part of the coun­try due to the rise in pre­cip­i­ta­tion. With ris­ing tem­per­a­tures, rain­fall in the moun­tains will increase at the expense of snow­fall: this will con­tribute to high­er win­ter flows in the Alps, the Pyre­nees and the Mas­sif Cen­tral. On an annu­al scale, there is no clear trend in riv­er flow, with the excep­tion of the south of France, where the mod­els clear­ly show a reduc­tion in annu­al flows.

Pro­ject­ed changes in mean sum­mer dis­charge for four con­trast­ing futures (Explore2 nar­ra­tives) under a sce­nario of high emis­sions at the end of the cen­tu­ry (base­line: 1976–2005) (medi­an esti­mate for all hydro­log­i­cal mod­els combined)

20% of the freshwater consumed in France comes from groundwater – the rest is taken from the surface2. Will this reserve also be affected by climate change?

Annu­al recharge of aquifers remains rel­a­tive­ly sta­ble between now and the end of the cen­tu­ry for both sources, except in the north of France where the mod­els project an increase.

In short, will some regions be more affected than others?

Water stress prob­lems will become more wide­spread in main­land France, par­tic­u­lar­ly in sum­mer, due to the com­bined effect of low­er rain­fall and high­er evap­o­tran­spi­ra­tion. But France is large enough for spa­tial con­trasts to emerge: we can iden­ti­fy areas that are more affect­ed, known as “hot spots”. The south-east (includ­ing Cor­si­ca) and south-west will be par­tic­u­lar­ly affect­ed by a drop in annu­al water resources. The sig­nal is less clear in terms of changes in sum­mer flows for the north of France.

What are the remaining uncertainties about the future of water resources in France?

France is on the bor­der­line between two major changes: in the north of Europe, rain­fall is set to increase as a result of cli­mate change; con­verse­ly, the Mediter­ranean basin is set to become dri­er. Is the tran­si­tion between these two trends tak­ing place in the north of France? Or in Bel­gium? It is still dif­fi­cult to get a clear answer from the cli­mate mod­els. Anoth­er source of uncer­tain­ty for the north of France is linked to the nat­ur­al dynam­ics of the region’s under­ground water tables: they store water in win­ter and release it in sum­mer, increas­ing the flow of rivers. Will this process com­pen­sate for the sum­mer droughts? Not all the mod­els agree.

These uncer­tain­ties are clear­ly rep­re­sent­ed in the Explore2 results. Cli­mate mod­els pro­vide us with infor­ma­tion about the pos­si­ble future cli­mate in France at the end of the cen­tu­ry under the impact of ris­ing green­house gas­es. We have there­fore cho­sen to retain four typ­i­cal cli­mates, the most con­trast­ing. These are our four “nar­ra­tives”: marked warm­ing and increased pre­cip­i­ta­tion (green); rel­a­tive­ly lit­tle change in the future (yel­low); sig­nif­i­cant warm­ing and strong sea­son­al con­trasts in pre­cip­i­ta­tion (pur­ple); severe warm­ing and extreme dry­ness in sum­mer (orange). For each hydro­log­i­cal indi­ca­tor, four maps are pre­sent­ed to illus­trate the pro­jec­tions accord­ing to each nar­ra­tive. This enables local actors to imag­ine the future of their area, tak­ing into account all the sci­en­tif­ic results.

What are the solutions available to them to adapt to these growing pressures on water resources?

The first lever is to use water spar­ing­ly. The results of Explore2 show the need to adapt to the impact of cli­mate change. We have made a dig­i­tal plat­form avail­able to every­one to facil­i­tate access to the results. They can be used as a start­ing point for devel­op­ing adap­ta­tion strate­gies. The exis­tence of the data has already been men­tioned in the Water Plan pre­sent­ed by the Gov­ern­ment in 2023, and some of the pro­jec­tions have been used by the Rhône-Méditer­ranée-Corse Water Agency to diag­nose the vul­ner­a­bil­i­ty of its ter­ri­to­ry to the effects of cli­mate change.

The hydro­log­i­cal pro­jec­tions for the worst-case GHG emis­sions sce­nario (RCP8.5), which I have detailed here, illus­trate the future if we do not mit­i­gate our impact on the cli­mate. This should also spur all play­ers to take action to lim­it glob­al warm­ing, and there are many ways in which we can do so.

Anaïs Marechal
1Sauquet, Éric; Evin, Guil­laume; Siauve, Sonia; Bor­nancin-Plantier, Audrey; Jacquin, Nat­acha; Arnaud, Patrick; Bérel, Maud; Bernus, Sébastien; Bon­neau, Jérémie; Branger, Flo­ra; Caballero, Yvan; Col­léoni, François; Col­let, Lila; Corre, Lola; Drouin, Agathe; Ducharne, Agnès; Fournier, Maïté; Gail­hard, Joël; Habets, Flo­rence; Hen­drickx, Frédéric; Héraut, Louis; Hingray, Benoît; Huang, Peng; Jaouen, Tris­tan; Jean­tet, Alex­is; Lani­ni, San­dra; Le Lay, Matthieu; Loudin, Sarah; Mag­a­nd, Claire; Mar­son, Paula; Mimeau, Louise; Mon­teil, Céline; Munier, Simon; Per­rin, Charles; Robin, Yoann; Rous­set, Fabi­enne; Soubey­roux, Jean-Michel; Strohmenger, Lau­rent; Thirel, Guil­laume; Toc­quer, Flo­re; Tram­blay, Yves; Vergnes, Jean-Pierre; Vidal, Jean-Philippe; Vrac, Math­ieu, 2024, “Mes­sages et enseigne­ments du pro­jet Explore2”, https://​doi​.org/​1​0​.​5​7​7​4​5​/​J​3XIPW, Recherche Data Gouv, V7
2https://​www​.sta​tis​tiques​.devel​oppe​ment​-durable​.gouv​.fr/​l​e​a​u​-​e​n​-​f​r​a​n​c​e​-​r​e​s​s​o​u​r​c​e​-​e​t​-​u​t​i​l​i​s​a​t​i​o​n​-​s​y​n​t​h​e​s​e​-​d​e​s​-​c​o​n​n​a​i​s​s​a​n​c​e​s​-​e​n​-2023

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