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Allied Second World War bombing raids disturbed atmosphere at edge of space

‘Astonishing’ discovery made by researchers looking at records kept by atmospheric scientists in the 1940s reveals ‘signatures of war’.
‘Astonishing’ discovery made by researchers looking at records kept by atmospheric scientists in the 1940s reveals ‘signatures of war’. ‘Astonishing’ discovery made by researchers looking at records kept by atmospheric scientists in the 1940s reveals ‘signatures of war’.

Shock waves from huge bombs dropped on Germany during the Second World War were powerful enough to alter the atmosphere at the edge of space, scientists have learned.

The allied bombing raids that began in 1942 caused unparalleled devastation on the ground as cities such as Dresden and Hamburg were reduced to rubble and ash.

But new research shows the massive explosions of heavy bombs that included the 10 tonne “Grand Slam” also disturbed the ionosphere hundreds of miles above the Earth.

The ionosphere, which extends from an altitude of about 50 kilometres (31 miles) to 1,000 kilometres (620 miles), is electrified by radiation from the sun and space.

At the height of the bombing raids the electrical charge it carried was significantly weakened, the study revealed.

US B-24s bombers flying through flak (National Museum/PA)

A team from the University of Reading made the discovery after comparing detailed records of the raids with data from British wartime scientists investigating the upper atmosphere.

Between 1943 and 1945, staff at the Radio Research Centre at Ditton Park, near Slough, fired a series of short wave radio pulses 100 to 300 kilometres above the Earth’s surface.

Echoes from the radio signals bouncing off the ionosphere layers revealed information about their height and electrical intensity. But unknown to the researchers, the data they recorded also bore a chilling hallmark of war.

Chris Scott, Professor of Space and Atmospheric Physics at the University of Reading, said: “The work at Slough was routinely analysing the height and intensity of these layers to understand how they vary, but what they didn’t realise at the time was that they actually contained the signatures of the  war itself.

“The images of neighbourhoods across Europe reduced to rubble due to war time air raids are a lasting reminder of the destruction that can be caused by man-made explosions. But the impact of these bombs way up in the Earth’s atmosphere has never been realised until now.

“It is astonishing to see how the ripples caused by man-made explosions can affect the edge of space. Each raid released the energy of at least 300 lightning strikes.”

The state of the ionosphere is known to be strongly influenced by solar activity and to a lesser extent natural phenomena such as thunderstorms, volcanic eruptions and earthquakes.

Its electrical properties affect radio communications as well as GPS systems, radio telescopes, and early warning radar.

Prof Scott said: “Because we know the energies involved in these explosions, that gives us a real quantifiable way of assessing how much energy is required to make the ionosphere wobble.”

The four-engine planes used in the allied raids were capable of carrying much larger bombs than those dropped in the Blitz by the German Luftwaffe’s two-engine aircraft.

A bomb load weighing as much as 2,000 tonnes could be dropped in a single raid.

University of Reading historian Professor Patrick Major said: “Aircrew involved in the raids reported having their aircraft damaged by the bomb shock waves, despite being above the recommended height.

“Residents under the bombs would routinely recall being thrown through the air by the pressure waves of air mines exploding, and window casements and doors would be blown off their hinges.

“The unprecedented power of these attacks has proved useful for scientists to gauge the impact such events can have hundreds of kilometres above the Earth, in addition to the devastation they caused on the ground.”

The research is published in the European Geosciences Union journal Annales Geophysicae.