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Volcanoes Can Reduce Greenhouse Gases

Дата публикации: 01-10-2026 06:00:29

New discoveries from the Hunga volcano show volcanoes can 'cancel' atmospheric methane (a greenhouse gas), bringing some optimism for climate scientists concerned about increased climate variability.

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New discoveries from the Hunga volcano show
volcanoes can ‘cancel’ atmospheric methane,
bringing some optimism for climate scientists
concerned about increased climate variability

When Volcanoes Clean the Sky:
Methane Destruction and Earth’s Self-Balancing Design

by Dr. Sarah Buckland-Reynolds

The Hunga volcano located in the South Pacific has been one full of surprises over the last few years and has appeared in headlines once more. Previously, this volcano caught headlines as its eruption was a surprise, and its 2022 eruption sent massive amounts of water vapour into the atmosphere, leading to many predictions of warming from this greenhouse gas, yet actual measurements years later showed that the opposite cooling effect was the outcome. This time, more research on Hunga focused on its effect on another atmospheric greenhouse gas: methane.

Satellite quantification of enhanced methane oxidation applied to the stratospheric plume following Hunga Tonga-Hunga Ha’apai eruption (Maarten et al., Nature Communications, 7 May 2026). Researchers documented a surprising discovery that the volcanic plume was actively destroying one of the most potent greenhouse gases: methane.

As the study’s lead author, Dr. Maarten van Herpen from Acacia Impact Innovation BV, explained in a press release by the University of Copenhagen:

“When we analysed the satellite images, we were surprised to see a cloud with a recordhigh concentration of formaldehyde. We were able to track the cloud for 10 days, all the way to South America. Because formaldehyde only exists for a few hours, this showed that the cloud must have been destroying methane continuously for more than a week.”

This finding has significant implications on discourse on climate variability processes, pointing to another apparent innate climate balancing mechanisms in the earth’s climate. For climate scientists concerned about increased climate variability, outlets have expressed that this observation also brings optimism for potential innovations for slowing accelerated warming.

Climate prognostications cannot possibly take into account all the factors involved.

Methane Oxidation:
Why this Process is Interesting in Climate Discourse

Methane (CH₄) is a Greenhouse Gas (GhG). Greenhouse gases are important to Earth’s habitability, as they are efficient in trapping longwave radiation from the sun, allowing just enough heat to be retained to support life. Given its importance in balance, natural habitats and creatures such as wetlands and cattle contribute to the cycle. However, accelerated increases in atmospheric greenhouse gas concentrations are what concerns many in the climate science community as causing what is frequently described as the ‘enhanced greenhouse effect,’ which is widely believed to be the cause of accelerated increases in earth’s average temperatures (and extreme events such as cyclones and droughts) since the industrial revolution.

Although methane is comparatively short-lived in the atmosphere compared with other greenhouse gases of concern (particularly CO₂), its role in warming concerns scientists as its potency is estimated to be over 80 times higher than CO2 in short-term scenarios of about 20 years. Due to its relatively short atmospheric stability (persisting for about a decade before breaking down into CO₂ and water vapour), current warming attributed to methane would therefore be driven almost entirely by recent emissions.

Given its potency, measures to reduce methane emissions and atmospheric concentrations of the gas are of importance to many climate scientists and have been the subject of international negotiations. Thus, scientists had begun exploring whether methane removal (including accelerating its natural breakdown) could serve as an “emergency brake” on the increases in its atmospheric concentration.

How the Volcano Destroyed Methane

While scientists have been facing several challenges to consider mechanisms for reducing methane emissions along with other GhGs, the Hunga Tonga eruption provided a dramatic natural demonstration, suggesting that natural mechanisms do exist toward restoring some ‘balance’. As Maarten et al (2026) reported, after the Hunga eruption, satellite instruments detected unusually high levels of formaldehyde (HCHO) in the volcanic plume. The presence of formaldehyde, being a short-lived intermediate in methane oxidation (surviving only a few hours), indicated ongoing methane destruction was occurring post-eruption. Its presence was found at a high altitude for more than ten days indicating continuous methane destruction.

As reported in their article, Maarten et al (2026) estimated that the volcano released about 330 gigagrams (Gg) of methane into the stratosphere. At the same time, the plume destroyed methane at a rate of 900 megagrams (Mg) per day (roughly equivalent to the daily emissions of two million cows).

As the authors described, the mechanism involved a surprising chemistry:

  1. Volcanic ash mixed with seawater blasted into the stratosphere.
  2. Sunlight striking this mixture triggered iron-chloride photochemistry, releasing chlorine atoms.
  3. As Chlorine is highly reactive, it attacks methane molecules, breaking them apart.

In their press release reported by the University of Copenhagen, Matthew Johnson (one of the researchers), described surprise at seeing this mechanism, as they had just recently discovered a similar mechanism from dust particle interactions with salt and sunlight. Quoting from the press release:

“According to the researchers, everything points to a very special process taking place— one they first discovered in 2023, but in a completely different part of the world.

They found that when dust from the Sahara is blown over the Atlantic Ocean, it mixes with sea salt from sea spray, forming small particles known as iron salt aerosols. When sunlight hits these aerosols, chlorine atoms are produced. These chlorine atoms react with methane and help break it down in the atmosphere. This discovery changed the scientific understanding of tropospheric chemistry.

“What is new—and completely surprising—is that the same mechanism appears to occur in a volcanic plume high up in the stratosphere, where the physical conditions are entirely different,” says Professor Matthew Johnson from the Department of Chemistry at the University of Copenhagen, one of the researchers behind both discoveries.

The 2022 eruption hurled enormous amounts of salty seawater into the stratosphere along with volcanic ash. The theory is that when sunlight hit this mixture, highly reactive chlorine was formed, helping to break down the methane released during the eruption. The visible evidence of this methane breakdown was the large amounts of formaldehyde detected in satellite images.”

Implications: Earth’s Capacity for Self-Balancing

The discovery suggests that Earth’s atmosphere may have more built-in resilience than is often assumed. As the Hunga volcano shows, eruptions, while destructive, can also trigger chemical processes that counteract greenhouse gases, alongside similar natural processes, such as blown desert dust.

There are several implications for this observation. Among the major ones of interest is the implication that this discovery may be yet another example of earth’s intrinsic processes that enable oscillating balances of climate. This means is based on atmospheric chemical reactions which are not limited to otherwise destructive eruptions, but also in dust plumes.

Climate scientists also find this observation remarkable because methane is estimated to be responsible for about one-third of recent atmospheric warming. While not being hailed as a ‘solution’ to ‘reverse’ warming, the reports suggest that the observation may inspire clean innovations, patterning these natural balancing processes.

The photochemical reactions join a long list of earth’s self-balancing mechanisms, including:

  • Forests as carbon sinks: Trees absorb CO₂, regulating climate.
  • Wetlands buffering floods: Natural hydrology reduces disaster risk.
  • Oceans absorbing carbon: Marine systems act as vast carbon reservoirs.
  • Soils sustaining food and livelihoods: Healthy soils store carbon and regulate water.

As UNEP itself has acknowledged, “the most effective climate solutions were embedded in creation long before humanity convened its first global climate conference, developed renewable energy technologies, or pledged net-zero commitments” (UNEP statement, 2025).

While this does not minimize the importance of responsible stewardship of creation that God ordained, these mechanisms remind us that Earth is not a passive victim of human activity but a dynamic system with God-given capacities for resilience.

Stewardship and Sovereignty

The Hunga Tonga eruption revealed a hidden resilience in Earth’s atmosphere. This natural process reduced greenhouse gas concentrations in a way previously unrecognized. From a theological perspective, discoveries like this point to God’s providence even in disasters as well as, in the case of the similarities in the effects of the dust photochemistry, the wisdom of God’s design. The atmosphere’s chemistry, the oceans’ buffering capacity, and the forests’ regulation of carbon are not accidents but part of a finely tuned creation.

These mechanisms do not absolve humanity of responsibility. Scripture teaches that humans are stewards, not owners, of creation. Genesis 2:15 records that God placed Adam in the garden “to work it and take care of it.” The existence of natural balancing processes is not a license for exploitation but a call to humility and responsibility.

The volcanic destruction of methane offers optimism, but it also underscores the fragility of Earth’s systems. Any attempt to manipulate atmospheric chemistry would require careful study to understand potential unintended effects. Thus, while we marvel at God’s sovereignty in embedding resilience into creation, we must also heed His mandate to care for the Earth responsibly.

Maarten et al’s study also advances climate science in practical ways, including introducing the need to recalibrate Earth’s methane budget. Scientists must now account for dust and volcanic ash as factors in methane destruction, reshaping global methane accounting.

Further research is needed to understand these processes fully and to explore whether they can be safely harnessed. As further research continues to uncover, we are reminded that Earth’s systems are not static but dynamic, and human ingenuity, guided by humility and stewardship, can align with natural processes to mitigate risks. The Earth, under God’s sovereignty, has capacities for renewal, and we are called to steward those capacities wisely.

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Dr. Sarah Buckland-Reynolds is a Christian, Jamaican, Environmental Science researcher, and journal associate editor. She holds the degree of Doctor of Philosophy in Geography from the University of the West Indies (UWI), Mona with high commendation, and a postgraduate specialization in Geomatics at the Universidad del Valle, Cali, Colombia. The quality of her research activity in Environmental Science has been recognized by various awards including the 2024 Editor’s Award from the American Meteorological Society for her reviewing service in the Weather, Climate and Society Journal, the 2023 L’Oreal/UNESCO Women in Science Caribbean Award, the 2023 ICETEX International Experts Exchange Award for study in Colombia. and with her PhD research in drought management also being shortlisted in the top 10 globally for the 2023 Allianz Climate Risk Award by Munich Re Insurance, Germany. Motivated by her faith in God and zeal to positively influence society, Dr. Buckland-Reynolds is also the founder and Principal Director of Chosen to G.L.O.W. Ministries, a Jamaican charitable organization which seeks to amplify the Christian voice in the public sphere and equip more youths to know how to defend their faith.  

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