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Water at the heart of global geopolitical issues

What future can we expect for water resources in France?

with 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​.stat​istiques​.develop​pe​ment​-dur​able​.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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