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The 1991 eruption sent up a cloud of ash 21km (13 miles) high. In volume this was 10 cubic km (2.4 cubic miles) of material.

The vast amount of aerosols and dust gradually spread through the stratosphere during the following year. Sulfur dioxide produced a global haze of sulfuric acid droplets. All this blocked out the sun. The amount of sunlight reaching the Earth's surface was reduced by 10%.

Temperatures in the northern hemisphere dropped by 0.5 C (0.9 F). At the same time temperatures in the stratosphere rose several degrees, because the dust and other particles there absorbed the sun's radiation (preventing it reaching the earth's surface). This cloud of aerosols from the explosion stayed in the stratosphere for three more years.

The eruption also lowered ozone levels. The winter ozone hole over Antarctica in 1992 was the largest ever.

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