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Climate change will lead to an increase in earthquakes

Christophe Larroque
Christophe Larroque
Lecturer at Université de Reims-Champagne Ardenne and at Geoazur Laboratory (CNRS/OCA/UniCA/IRD)
Marco Bohnoff
Marco Bohnhoff
Professor of Experimental Seismology and Drilling at Freie Universität of Berlin
Key takeaways
  • For decades and centuries to come, global warming will continue to accelerate the triggering of certain earthquakes.
  • Weather conditions influence seismic activity: in 2020, storm Alex caused intense rainfall in south-eastern France, leading to 188 magnitude 2 earthquakes in the Mercantour National Park in the following 100 days.
  • The relationship between weather and seismicity is based on various mechanisms, where small variations in stress can be enough to trigger earthquakes.
  • Global warming is intensifying these meteorological phenomena by increasing temperatures at the Earth’s surface, speeding up the melting of glaciers, and accentuating extreme precipitation, cyclones and rising sea levels.
  • There is therefore an urgent need to reduce greenhouse gas emissions to limit the number of earthquakes linked to climate change.

Every year, dozens of major earth­quakes1 occur around the world. These events can cause the death2 of hun­dreds of thou­sands of peo­ple, as was the case recent­ly in 2010 (226,000 deaths) and 2004 (227,000 deaths). Earth­quakes are trig­gered by an abrupt slip along a fault – known as a frac­ture – in the Earth’s crust, i.e. the first few kilo­me­tres beneath our feet. This slip occurs when the stress­es on the fault exceed a rup­ture thresh­old, par­tic­u­lar­ly due to the move­ments of the tec­ton­ic plates. But in recent years, a research top­ic has emerged in the sci­en­tif­ic com­mu­ni­ty: could cli­mate change caused by human activ­i­ties influ­ence earthquakes?

“The dis­rup­tion caused by human activ­i­ties is so intense and wide­spread that it is felt right across the plan­et – we even talk about the Anthro­pocene” stress­es Christophe Lar­roque. “We’re won­der­ing about the impact on seis­mic­i­ty.” Mar­co Bohn­hoff com­ments, “This is a new sub­ject and there are very few research groups work­ing on it, but there is grow­ing inter­est.” In an arti­cle pub­lished last May, Mar­co Bohn­hoff and his col­leagues sum­marised what is cur­rent­ly known3: over sev­er­al decades and cen­turies, human activ­i­ties will mod­i­fy the seis­mic clock on faults, trig­ger­ing an increas­ing num­ber of small and large earth­quakes. In oth­er words, where faults are on the verge of rup­ture, ready to slip and gen­er­ate an earth­quake, cli­mate change could be the trig­ger, accel­er­at­ing the occur­rence of the earthquake.

The influence of weather on earthquakes

It is now clear that the weath­er influ­ences earth­quakes. In 2020, France was swept by storm Alex, which gen­er­at­ed very heavy rain­fall in the south-east of the coun­try, up to 600 mm in less than 24 hours. Over the next 100 days, 188 earth­quakes of up to mag­ni­tude 2 – a mag­ni­tude too weak to be felt by the gen­er­al pub­lic – were record­ed in the Tinée val­ley, in the Mer­can­tour nation­al park4. “This is a sig­nif­i­cant find­ing: we record­ed as many earth­quakes in this area in three months as we had in 5 years” points out Christophe Larroque.

The first obser­va­tions of the influ­ence of weath­er on seis­mic­i­ty date back to the ear­ly 2000s. In France, in 2002, after rain­fall as intense as dur­ing Storm Alex, an increase in seis­mic activ­i­ty was record­ed in the fol­low­ing months in west­ern Provence5. In 2005, an unusu­al series of 47 earth­quakes was record­ed in the space of just 12 hours in cen­tral Switzer­land, fol­low­ing intense rain­fall (300 mm in 3 days)6. Anoth­er exam­ple: in Nepal, a team record­ed a low­er num­ber of earth­quakes in sum­mer (-37%) than in win­ter, sug­gest­ing that mon­soons influ­ence seis­mic­i­ty7.

Exam­ples also exist for oth­er weath­er events. Cal­i­for­nia, for exam­ple, has alter­nat­ing wet and dry sea­sons when snow and water accu­mu­late in moun­tains, lakes and reser­voirs. This sea­son­al pat­tern has been shown to mod­i­fy seis­mic­i­ty rates in the region8. And in Turkey, oscil­la­tions in the lev­el of the Sea of Mar­mara – asso­ci­at­ed with sea­son­al vari­a­tions – also cor­re­late with the num­ber of earth­quakes9. “So far, the earth­quakes linked to mete­o­ro­log­i­cal events have main­ly been of low mag­ni­tude, although this does not rule out the pos­si­bil­i­ty of larg­er mag­ni­tude earth­quakes in the future” explains Christophe Lar­roque. “This pos­es real chal­lenges in terms of obser­va­tion, since we need to deploy a high-qual­i­ty seis­mo­log­i­cal record­ing net­work to accu­rate­ly record these small earth­quakes. In recent years, the improve­ment and mul­ti­pli­ca­tion of seis­mo­log­i­cal net­works has improved our understanding.”

The mechanisms involved in the relationship between weather and earthquakes

What mech­a­nisms explain this cor­re­la­tion between weath­er and seis­mic­i­ty? “A num­ber of process­es are in play, and it is dif­fi­cult to iden­ti­fy which ones are respon­si­ble” replies Christophe Lar­roque. Regard­ing storm Alex, Christophe Lar­roque and his col­leagues have just pub­lished a ground-break­ing analy­sis that brings togeth­er a num­ber of dif­fer­ent dis­ci­plines. “We pin­point­ed the pre­cise loca­tion of the earth­quakes, traced their migra­tion over time, and mod­elled var­i­ous hypothe­ses to under­stand the process­es involved” explains Christophe Lar­roque. For exam­ple, the team has shown that the rain gen­er­at­ed excess flu­id pres­sure that prop­a­gat­ed at depth – known as a pres­sure front – until it desta­bilised a fault that was already under stress. The fault then began to slip until it trig­gered small clus­ters of earthquakes.

It is impor­tant to under­stand that small vari­a­tions in stress can be enough to trig­ger earth­quakes. While the pres­sure front gen­er­at­ed by storm Alex is at the root of the unusu­al seis­mic­i­ty in the region, mete­o­ro­log­i­cal events can mod­i­fy stress­es local­ly through oth­er mech­a­nisms. One study looked at the effects of typhoon Morakot in Tai­wan in 200910. The intense rain­fall caused more than 10,000 land­slides and a very large amount of rock and sed­i­ment to be trans­port­ed in rivers. These sur­face mass move­ments increased stress­es on faults, explain­ing the sig­nif­i­cant increase in the fre­quen­cy of sur­face earth­quakes for two and a half years after the typhoon hit. Anoth­er exam­ple: in Cal­i­for­nia, sea­son­al vari­a­tions in seis­mic­i­ty are main­ly linked to stress­es gen­er­at­ed by the weight of water accu­mu­lat­ing on the sur­face dur­ing the wet sea­son11.

Yet all these mete­o­ro­log­i­cal events are influ­enced by cli­mate change linked to human activ­i­ties and will be even more so in the future. Ris­ing tem­per­a­tures at the Earth’s sur­face are caus­ing ice caps to melt rapid­ly, increas­ing the inten­si­ty of extreme pre­cip­i­ta­tion and cyclones, as well as glob­al sea lev­els12. All these sur­face changes are mod­i­fy­ing stress­es on faults locally.

A study of earth­quakes on the Kore­an penin­su­la over the last 650,000 years shows a cor­re­la­tion between seis­mic­i­ty and the end of the var­i­ous ice ages: with each deglacia­tion, the melt­ing of the ice caus­es a rapid rise in sea lev­el and an increase in seis­mic activ­i­ty in the region13. With glob­al sea lev­els already hav­ing risen by 0.2m since 1901 and set to rise by a fur­ther 1m by 2100, the con­se­quences could be sig­nif­i­cant. Some esti­mate that a rise of 1m could increase the pres­sure on all the oceans (i.e. 70% of the earth’s sur­face) enough to trig­ger earth­quakes on many faults that are already close to rup­ture. “Ris­ing sea lev­els will in most cas­es accel­er­ate the onset of earth­quakes, though in oth­er cas­es it will delay them” con­cludes Mar­co Bohn­hoff. “In this case, more ener­gy will accu­mu­late on the faults and the earth­quakes will be stronger. This will affect the peo­ple who live on the coast, and we urgent­ly need to reduce green­house gas emis­sions to lim­it the num­ber of earth­quakes caused by cli­mate change.”

Anaïs Marechal
1“Data Page: Num­ber of sig­nif­i­cant earth­quakes”, part of the fol­low­ing pub­li­ca­tion: Han­nah Ritchie and Pablo Rosa­do (2022) – “Nat­ur­al Dis­as­ters”. Data adapt­ed from Nation­al Geo­phys­i­cal Data Cen­ter / World Data Ser­vice. Retrieved from https://​our​worldin​da​ta​.org/​g​r​a​p​h​e​r​/​s​i​g​n​i​f​i​c​a​n​t​-​e​a​r​t​h​q​uakes [online resource]
2“Data Page: Deaths from earth­quakes”, part of the fol­low­ing pub­li­ca­tion: Han­nah Ritchie and Pablo Rosa­do (2022) – “Nat­ur­al Dis­as­ters”. Data adapt­ed from Nation­al Geo­phys­i­cal Data Cen­ter / World Data Ser­vice. Retrieved from https://​our​worldin​da​ta​.org/​g​r​a​p​h​e​r​/​e​a​r​t​h​q​u​a​k​e​-​d​eaths [online resource]
3Mar­co Bohn­hoff, Patri­cia Martínez-Garzón, Yehu­da Ben-Zion; Glob­al Warm­ing Will Increase Earth­quake Haz­ards through Ris­ing Sea Lev­els and Cas­cad­ing Effects. Seis­mo­log­i­cal Research Let­ters, 2024; 95 (5): 2571–2576. doi: https://​doi​.org/​1​0​.​1​7​8​5​/​0​2​2​0​2​40100
4Jacque­mond, L., Godano, M., Cap­pa, F., & Lar­roque, C. (2024). Inter­play between flu­id intru­sion and aseis­mic stress per­tur­ba­tions in the onset of earth­quake swarms fol­low­ing the 2020 Alex extreme rain­storm. Earth and Space Sci­ence, 11,e2024EA003528, https://​doi​.org/​1​0​.​1​0​2​9​/​2​0​2​4​E​A​0​03528
5Alex­is Rigo, Nicole Béthoux, Frédéric Mas­son, Jean-François Ritz, Seis­mic­i­ty rate and wave-veloc­i­ty vari­a­tions as con­se­quences of rain­fall: The case of the cat­a­stroph­ic storm of Sep­tem­ber 2002 in the Nîmes Fault region (Gard, France), Geo­phys­i­cal Jour­nal Inter­na­tion­al, Vol­ume 173, Issue 2, May 2008, Pages 473–482, https://doi.org/10.1111/j.1365–246X.2008.03718.x
6S. Husen, C. Bach­mann, D. Gia­r­di­ni, Local­ly trig­gered seis­mic­i­ty in the cen­tral Swiss Alps fol­low­ing the large rain­fall event of August 2005, Geo­phys­i­cal Jour­nal Inter­na­tion­al, Vol­ume 171, Issue 3, Decem­ber 2007, Pages 1126–1134, https://doi.org/10.1111/j.1365–246X.2007.03561.x
7Bollinger, L.,  F. Per­ri­er,  J.-P. Avouac,  S. Sap­ko­ta,  U. Gau­tam, and  D. R. Tiwari (2007), Sea­son­al mod­u­la­tion of seis­mic­i­ty in the Himalaya of Nepal, Geo­phys. Res. Lett.,  34, L08304, doi:10.1029/2006GL029192.
8Bollinger, L.,  F. Per­ri­er,  J.-P. Avouac,  S. Sap­ko­ta,  U. Gau­tam, and  D. R. Tiwari (2007), Sea­son­al mod­u­la­tion of seis­mic­i­ty in the Himalaya of Nepal, Geo­phys. Res. Lett.,  34, L08304, doi:10.1029/2006GL029192.
9Martínez-Garzón, P.,  Beroza, G. C.,  Boc­chi­ni, G. M., &  Bohn­hoff, M. (2023).  Sea lev­el changes affect seis­mic­i­ty rates in a hydrother­mal sys­tem near Istan­bul. Geo­phys­i­cal Research Let­ters,  50, e2022GL101258. https://​doi​.org/​1​0​.​1​0​2​9​/​2​0​2​2​G​L​1​01258
10Steer, P., Jean­det, L., Cubas, N. et al. Earth­quake sta­tis­tics changed by typhoon-dri­ven ero­sion. Sci Rep 10, 10899 (2020). https://doi.org/10.1038/s41598-020–67865‑y
11John­son, C. W.,  Fu, Y., &  Bürgmann, R. (2017).  Stress mod­els of the annu­al hydros­pher­ic, atmos­pher­ic, ther­mal, and tidal load­ing cycles on Cal­i­for­nia faults: Per­tur­ba­tion of back­ground stress and changes in seis­mic­i­ty. Jour­nal of Geo­phys­i­cal Research: Sol­id Earth, 122,  10,605–10,625. https://​doi​.org/​1​0​.​1​0​0​2​/​2​0​1​7​J​B​0​14778
12IPCC, 2023: Sum­ma­ry for Pol­i­cy­mak­ers. In: Cli­mate Change 2023: Syn­the­sis Report. Con­tri­bu­tion of Work­ing Groups I, II and III to the Sixth Assess­ment Report of the Inter­gov­ern­men­tal Pan­el on Cli­mate Change [Core Writ­ing Team, H. Lee and J. Romero (eds.)]. IPCC, Gene­va, Switzer­land, pp. 1–34, doi: 10.59327/IPCC/AR6-9789291691647.001
13Man-Jae Kim, Hee-Kwon Lee, Long-term pat­terns of earth­quakes influ­enced by cli­mate change: Insights from earth­quake recur­rence and stress field changes across the Kore­an Penin­su­la dur­ing inter­glacial peri­ods, Qua­ter­nary Sci­ence Reviews, Vol­ume 321, 2023, 108369, ISSN 0277–3791, https://​doi​.org/​1​0​.​1​0​1​6​/​j​.​q​u​a​s​c​i​r​e​v​.​2​0​2​3​.​1​08369.

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