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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​.sta​tis​tiques​.deve​lop​pe​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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