Major volcanic eruptions episodically disrupted the continuity of polar warming through aerosol forcing

Abstract The polar regions are warming rapidly, exceeding the global average due to greenhouse gas emissions from human activities. Using CMIP6 simulations, HadCRUT5 data, and MERRA-2 aerosol records, this study shows that major 20th-century volcanic eruptions, Agung (1963), El Chichón (1982), and Pinatubo (1991) temporarily offset polar warming through sulfate-induced cooling. The Agung eruption suppressed Arctic surface air temperature anomalies for approximately 4–5 years (1964–1968), El Chichón for a similar duration (1983–1987), and Pinatubo for about 4–5 years (1992–1996), demonstrating a consistent multi-year cooling response following each event. Without these eruptions, Arctic surface air temperature anomalies would have increased by up to 0.5 °C, whereas volcanic activity caused short-term cooling ranging from −0.07 °C to −0.4 °C. Arctic minimum temperatures ( $${T}_{\min }$$ T min ) are rising faster than maximum temperatures ( $${T}_{\max }$$ T max ), indicating asymmetric warming. In contrast, Antarctic responses were weaker, moderated by oceanic and atmospheric dynamics. Collectively, these eruptions produced episodic multi-year cooling that temporarily interrupted the ongoing Arctic warming trajectory, with warming resuming as volcanic aerosol forcing diminished. Spatial patterns reveal pronounced warming in the central Arctic, Greenland, and Siberia in the absence of volcanic forcing, highlighting the role of eruptions in modulating polar warming and providing insights relevant to future geoengineering considerations.

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Publication Details

Journal
npj Clean Air
Published
2026-11-01
DOI
https://doi.org/10.1038/s44407-026-00111-3
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
0.00

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article

Major volcanic eruptions episodically disrupted the continuity of polar warming through aerosol forcing

Scott Osprey, Rui Song, Basudev Swain, R. G. Grainger et al.
npj Clean Air
Climate variability and models
article

Major volcanic eruptions episodically disrupted the continuity of polar warming through aerosol forcing

Scott Osprey, Rui Song, Basudev Swain, R. G. Grainger, Marco Vountas
article en

Abstract

Abstract The polar regions are warming rapidly, exceeding the global average due to greenhouse gas emissions from human activities. Using CMIP6 simulations, HadCRUT5 data, and MERRA-2 aerosol records, this study shows that major 20th-century volcanic eruptions, Agung (1963), El Chichón (1982), and Pinatubo (1991) temporarily offset polar warming through sulfate-induced cooling. The Agung eruption suppressed Arctic surface air temperature anomalies for approximately 4–5 years (1964–1968), El Chichón for a similar duration (1983–1987), and Pinatubo for about 4–5 years (1992–1996), demonstrating a consistent multi-year cooling response following each event. Without these eruptions, Arctic surface air temperature anomalies would have increased by up to 0.5 °C, whereas volcanic activity caused short-term cooling ranging from −0.07 °C to −0.4 °C. Arctic minimum temperatures ( $${T}_{\min }$$ T min ) are rising faster than maximum temperatures ( $${T}_{\max }$$ T max ), indicating asymmetric warming. In contrast, Antarctic responses were weaker, moderated by oceanic and atmospheric dynamics. Collectively, these eruptions produced episodic multi-year cooling that temporarily interrupted the ongoing Arctic warming trajectory, with warming resuming as volcanic aerosol forcing diminished. Spatial patterns reveal pronounced warming in the central Arctic, Greenland, and Siberia in the absence of volcanic forcing, highlighting the role of eruptions in modulating polar warming and providing insights relevant to future geoengineering considerations.

npj Clean AirVol. 2(1)
University of Bremen (DE), University of Oxford (GB)
UK Research and Innovation, Natural Environment Research Council, National Centre for Earth Observation
Climate action
Openalex Percentile: Top 17%
Climate variability and models
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