Volcanic eruption played part in Napoleon Bonaparte's defeat: Study

London, PTI | Updated : 27 August 2018, 05:20 PM
Volcanic eruption played part in Napoleon Bonaparte's defeat: Study (Photo:Twitter/@IndonesiaWorld5)
Volcanic eruption played part in Napoleon Bonaparte's defeat: Study (Photo:Twitter/@IndonesiaWorld5)

A volcano that erupted in Indonesia in 1815 and caused poor global weather may have been partly responsible for the defeat of French Emperor Napoleon Bonaparte at the Battle of Waterloo, changing the course of European history.

Historians know that rainy and muddy conditions helped the Allied army defeat Napoleon, according to the researchers from Imperial College London in the UK.

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Two months prior to the June 1815 event, a volcano named Mount Tambora erupted on the Indonesian island of Sumbawa, killing 100,000 people and plunging the Earth into a 'year without a summer' in 1816.

Researchers found that electrified volcanic ash from eruptions can 'short-circuit' the electrical current of the ionosphere- the upper level of the atmosphere that is responsible for cloud formation.

The findings, published in the journal Geology, could confirm the suggested link between the eruption and Napoleon's defeat.

The Tambora eruption short-circuited the ionosphere, ultimately leading to a pulse of cloud formation. This brought heavy rain across Europe that contributed to Napoleon's defeat.

The study shows that eruptions can hurl ash much higher than previously thought into the atmosphere up to 100 kilometres above ground.

A series of experiments showed that that electrostatic forces could lift ash far higher than by buoyancy alone.

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Researchers created a model to calculate how far charged volcanic ash could levitate, and found that particles smaller than 0.2 millionths of a metre in diameter could reach the ionosphere during large eruptions.

"Volcanic plumes and ash both can have negative electrical charges and thus the plume repels the ash, propelling it high in the atmosphere," said Matthew Genge from Imperial College London.

 "The effect works very much like the way two magnets are pushed away from each other if their poles match," he said.

The experimental results are consistent with historical records from other eruptions.

Weather records are sparse for 1815, so to test his theory, researchers examined weather records following the 1883 eruption of another Indonesian volcano, Krakatau.

The data showed lower average temperatures and reduced rainfall almost immediately after the eruption began, and global rainfall was lower during the eruption than either period before or after.

He also found reports of ionosphere disturbance after the 1991 eruption of Mount Pinatubo, Philippines, which could have been caused by charged ash in the ionosphere from the volcano plume.

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A special cloud type appeared more frequently than usual following the Krakatau eruption. Noctilucent clouds are rare and luminous, and form in the ionosphere.

Genge suggests these clouds therefore provide evidence for the electrostatic levitation of ash from large volcanic eruptions.

"Vigo Hugo in the novel Les Miserables said of the Battle of Waterloo: 'an unseasonably clouded sky sufficed to bring about the collapse of a World.' Now we are a step closer to understanding Tambora's part in the Battle from half a world away," he said.

First Published: Monday, August 27, 2018 02:12 PM
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