Climate science

Volcanic eruptions and weather

A single volcanic eruption can cool the entire planet by 1°F for years. Here is the science of how the atmosphere responds.

The basic mechanism

  1. Large volcanic eruption ejects SO2 (sulfur dioxide) into stratosphere.
  2. SO2 combines with water to form sulfate aerosol droplets.
  3. Aerosols reflect solar radiation back to space.
  4. Global surface cools.
  5. Aerosols remain in stratosphere 1-3 years before falling out.
  6. Cooling effect fades as aerosols clear.

What matters for climate

The Volcanic Explosivity Index (VEI)

VEI 1
Kilauea. Little climate impact.
VEI 2
Small ashfall.
VEI 3
Regional impact.
VEI 4
Significant regional cooling possible.
VEI 5
Historic impact scale.
VEI 6
Global cooling, months-year timescale. 1991 Pinatubo.
VEI 7
Historic. 1815 Tambora. Multi-year global impact.
VEI 8
Supervolcano. Toba (74,000 years ago).

The 1815 Tambora eruption

The largest documented volcanic eruption of modern era.

The Year Without a Summer

The 1883 Krakatoa eruption

The 1991 Pinatubo eruption

The largest volcanic eruption of the 20th century.

Recent eruptions

1980 Mount St. Helens
VEI 5. Regional not global. 57 dead.
2010 Eyjafjallajökull (Iceland)
VEI 4. Local. Grounded European aviation.
2011 Puyehue-Cordón Caulle (Chile)
VEI 5. Southern Hemisphere impacts.
2022 Hunga Tonga-Hunga Ha'apai
VEI 5-6. Submarine. Injected water vapor to stratosphere. Small stratospheric warming.

The Hunga Tonga case

The 2022 Tonga eruption was unusual.

Volcanic forcing on climate

Volcanic geoengineering proposals

The volcanic weather ripple effects

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