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Climate change will also have an impact on volcanic eruptions

Virginie Pinel
Virginie Pinel
Research Director of Volcanology at Institut de Recherche pour le Développement (IRD)
Thomas-Aubry
Thomas Aubry
Senior Lecturer in the Department of Earth Science at the University of Exeter
Key takeaways
  • Climate change is altering geological systems, including volcanic eruptions.
  • Melting glaciers, for example, can cause magma to rise to the surface, while rising sea levels can reduce magma production at depth.
  • Over time, certain volcanic regions can expect an increase in eruptions and secondary hazards (lahars).
  • However, it is still difficult to attribute a particular eruption to climate change.

How does climate change influence geological phenomena such as volcanic eruptions?

Vir­ginie Pinel. For an erup­tion to occur, magma must reach the earth’s sur­face. How­ever, changes on the sur­face can encour­age the pro­duc­tion of magma at depth or facil­it­ate its ascent1. Let’s take the lat­ter example: magma is less dense than the sur­round­ing rocks, so it rises to the sur­face thanks to Archimedes’ law of buoy­ancy [edit­or­’s note: just like oil immersed in water]. If the load above the magma cham­ber is reduced, the magma can rise faster. This is pre­cisely what hap­pens when gla­ciers melt as a res­ult of human-induced cli­mate change. When a gla­ci­er decreases in thick­ness or width, a magma reser­voir at depth can rup­ture and magma can rise to the sur­face. Espe­cially if the vol­cano is already close to eruption!

And what about magma production at depth?

VP. The melt­ing of gla­ciers over large areas increases magma pro­duc­tion at depth. Con­versely, for sub­mar­ine vol­ca­noes, rising sea levels linked to human-induced cli­mate change are increas­ing pres­sure on magma cham­bers. This could reduce magma production.

Have these phenomena already been observed and measured?

VP. Yes, par­tic­u­larly through geo­lo­gic­al evid­ence of past vol­can­ic activ­ity. We are see­ing changes in vol­can­ic activ­ity linked to past cli­mate change. In Ice­land, for example, vol­can­ic erup­tion rates were 30 to 50 times high­er than they are today, fol­low­ing major degla­ci­ation in the past (the last of which took place 10,000 years ago). But there are also effects on present-day vol­can­ism, par­tic­u­larly in Ice­land, where sea­son­al erup­tions are linked to vari­ations in snow depth.

For several years now, attribution studies have been determining the impact of climate change on the probability of extreme weather events. What about volcanic eruptions?

Thomas J. Aubry. It’s still dif­fi­cult to attrib­ute the occur­rence of an erup­tion to cli­mate change. We can attrib­ute the trig­ger­ing of cer­tain erup­tions to pre­cip­it­a­tion, par­tic­u­larly on vol­ca­noes whose erupt­ive his­tory and magma sys­tem are well known. Pre­cip­it­a­tion – also mod­i­fied by cli­mate change – can infilt­rate deep under­ground and react with the magma sys­tem to trig­ger an erup­tion. But for a par­tic­u­lar erup­tion, it is com­plic­ated to reli­ably determ­ine the dual link between erup­tion and pre­cip­it­a­tion, and between pre­cip­it­a­tion and cli­mate change.

Does climate change influence the eruption once it has started?

TA. Yes, many erupt­ive pro­cesses are influ­enced. In par­tic­u­lar, sur­face hydro­logy has a huge impact on erupt­ive style. If the magma encoun­ters an ice cap or lake on its way to the sur­face, the erup­tion releases much more energy, and the vol­can­ic plume reaches a great­er height. Cli­mate change influ­ences this sur­face hydrology.

The oth­er effect of cli­mate on erup­tions con­cerns the rise of the vol­can­ic plume in the atmo­sphere. Its height is mainly con­trolled by the intens­ity of the erup­tion (men­tioned above), but also by tem­per­at­ure and dens­ity gradi­ents in the atmo­sphere. In trop­ic­al zones, cli­mate change is modi­fy­ing the tro­po­sphere – the low­est 16 kilo­met­ers of the atmo­sphere – in such a way that plumes rise less. Plume heights could fall by 1 to 2 km by the end of the cen­tury if we con­tin­ue to emit green­house gases. Out­side the trop­ics, the impact of cli­mate change on plumes is linked to wind pat­terns, which vary greatly accord­ing to region and altitude.

Are certain volcanic regions more affected by climate change?

TA. We are cur­rently work­ing to map the vol­ca­noes most sens­it­ive to cli­mate change. Roughly speak­ing, we know that this con­cerns regions where gla­ciers are melt­ing fast, such as Ice­land or Chile, as well as vol­ca­noes that are heav­ily affected by pre­cip­it­a­tion, such as in Indone­sia. A study pub­lished in 20222 shows that 716 vol­ca­noes world­wide – or 58% of act­ive above-ground vol­ca­noes – will be affected by more extreme pre­cip­it­a­tion as glob­al tem­per­at­ures con­tin­ue to rise. We can there­fore expect poten­tially more eruptions.

VP. The oth­er effect of extreme pre­cip­it­a­tion is an increase in sec­ond­ary haz­ards, par­tic­u­larly lahars. Melt­ing ice and extreme rain­fall can trig­ger these mud­flows com­posed of ash from former vol­can­ic erup­tions: this phe­nomen­on con­trib­utes sig­ni­fic­antly to the num­ber of vol­cano-related deaths world­wide. Many vol­can­ic sites are affected.

Does this have any implications for volcanic risk management?

TA. In regions par­tic­u­larly sens­it­ive to cli­mate change, we believe that the fre­quency and intens­ity of erup­tions will change as glob­al warm­ing increases. Gov­ern­ment agen­cies are already address­ing these changes. In the past, cli­mate change has had a dra­mat­ic effect on vol­can­ic erup­tions. But it’s import­ant to keep things in per­spect­ive: past cli­mate changes were on a much lar­ger scale, so we don’t expect to see such dra­mat­ic changes. On the oth­er hand, one of our motiv­a­tions for work­ing on this sub­ject is to high­light the con­sequences of our activ­it­ies. If we don’t mit­ig­ate cli­mate change suf­fi­ciently, we’ll go so far as to modi­fy geo­lo­gic­al sys­tems. I find that unbelievable…

VP. As far as risk man­age­ment is con­cerned, the effects of cli­mate change are also hav­ing an impact on erup­tion fore­cast­ing. Melt­ing ice and changes in pre­cip­it­a­tion induce ground dis­place­ments: yet it is the ground dis­place­ments linked to vol­can­ic pro­cesses – such as the rising of magma – that enable erup­tions to be anti­cip­ated. The effects of cli­mate change are dis­rupt­ing the signals.

How widely known are the effects of climate change on volcanic activity?

TA. The effects of vol­can­ic activ­ity on cli­mate are well known. It is cru­cial to under­stand the impact of nat­ur­al pro­cesses on cli­mate in order to meas­ure the effects of human activ­it­ies. The oppos­ite has been far less stud­ied. Only the link between degla­ci­ation and vol­can­ic erup­tions has been widely explored thanks to geo­lo­gic­al records.

VP. The dif­fi­culty in this field of study lies in the time scale. Vol­can­ic sys­tems are built up over sev­er­al hun­dred thou­sand years, where­as cli­mate change takes place over a few dec­ades. We don’t yet have enough hind­sight to have a clear vis­ion of the changes under­way in vol­can­ic activ­ity. Nev­er­the­less, cli­mate change rep­res­ents an oppor­tun­ity for us to bet­ter under­stand the factors that mod­u­late and trig­ger erup­tions, like a life-size experiment.

Anaïs Marechal
1Aubry, T.J., Far­quhar­son, J.I., Row­ell, C.R. et al. Impact of cli­mate change on vol­can­ic pro­cesses: cur­rent under­stand­ing and future chal­lenges. Bull Vol­can­ol 84, 58 (2022). https://doi.org/10.1007/s00445-022–01562‑8
2Far­quhar­son Jam­ie I. and Ame­lung Falk (2022) Vol­can­ic haz­ard exacer­bated by future glob­al warm­ing-driv­en increase in heavy rain­fall, R. Soc. Open Sci.9220275. http://​doi​.org/​1​0​.​1​0​9​8​/​r​s​o​s​.​2​20275

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