Why Does A Nuclear Explosion Create A Mushroom Cloud?

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A nuclear (or any sufficiently powerful) explosion creates a mushroom cloud because it suddenly releases an enormous amount of heat. The fireball, much hotter than the surrounding air, rises rapidly as a buoyant plume, drawing cooler air and debris up its stem (Rayleigh-Taylor instability). When it hits a stable layer of the atmosphere - typically the tropopause - it can rise no further and spreads out sideways, forming the cap of the “mushroom”. Big volcanic eruptions and large conventional blasts can produce the same shape.

If you’ve ever looked up pictures of nuclear explosions on the Internet, you have likely observed something rather intriguing about them: regardless of the type of explosion or where they occur, all of them appear to form a ‘mushroom cloud’ in the sky.

Nuclear war explosion in city mushroom cloud
Photo Credit : Razvan Ionut Dragomirescu / Shutterstock

One noteworthy aspect of nuclear explosions is that they’re markedly different from regular explosions, i.e., the ones caused by dynamites, grenades, missiles etc. So, why do nuclear explosions cause such dramatic and consistent formations in the sky?


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What’s A Mushroom Cloud?

A mushroom cloud is an iconic mushroom-shaped cloud of smoke/debris that forms in the sky following an extremely large explosion. Although it’s usually associated with a nuclear explosion, a mushroom cloud can be formed following any event that results in a rapid release of heat, like a volcano, a forest fire, an impact event (a large-scale collision between astronomical objects) or a particularly powerful explosion (like those caused by vacuum bombs).

mushroom-clouds-can-only-be-formed-by-nuclear-explosions-meme

Why Do Nuclear Explosions Cause Mushroom Clouds?

A particularly powerful explosion is accompanied by a sudden release of a great deal of heat. This heat interacts with the surrounding air, making it hotter and less dense, resulting in what’s known as Rayleigh–Taylor instability in scientific circles. Simply put, it says that when two fluids of different densities (and thus subject to different accelerations) interact, the lighter fluid pushes on the denser fluid.

Apart from the mushroom cloud itself, the suspension of water atop oil, volcanic eruptions, jet streams of winds that regulate Earth’s climate, and supernovae explosions are some instances where Rayleigh-Taylor instability comes into play.

crab-nebula
An example of RT instability in the Crab Nebula, a supernova remnant and pulsar wind nebula in the constellation of Taurus (Image Source: Wikimedia Commons)

As mentioned earlier, the sudden release of energy following an explosion heats up the surrounding air which then starts to expand. The giant fireball created in the initial stages of the explosion is incredibly hot, with temperatures running up to millions of degrees of Celsius, which is akin to what you could expect to find in the middle of the Sun!

Now, the hot air within the fireball rises rapidly in the air, creating a vacuum that is then rapidly filled by the surrounding air, which also expands and starts to rise. This process continues for quite some time, during which the fireball continues to quickly rise through the sky.

As the fireball continues to rise, it experiences resistance from the air on top of it, which pushes it down sideways. This leads to the flattening of the top of the cloud, which then appears like the cap of a mushroom. The displaced gas, which is at a lower temperature than the air in the center of the column, trickles down the sides of the column, only to get sucked back in by the rising column to travel upwards again.

mashrum-cloud-formation

This is the reason why the edges of an explosion’s fireball appear to be curling constantly. Since a nuclear explosion occurs at a much larger scale than regular explosions, the fireball it creates is proportionally gigantic.

End Of The Fireball’s Journey

The fireball continues to rise until it reaches a stable layer of the atmosphere, typically the tropopause - the boundary between the troposphere and the stratosphere, around 10-17 km up depending on latitude. There the temperature stops dropping with altitude (and even rises again, thanks to ozone absorbing solar UV), and the buoyant plume can no longer punch its way up. The rising air stops abruptly and spreads out horizontally, making a perfect top for the mushroom cloud.

mushroom-cloud
The mushroom cloud created by the eruption of Redoubt Volcano on April 21, 1990. Note that the rising air stops abruptly and spreads out horizontally after attaining a particular altitude (Photo Credit : Wikipedia.org)

How Big Is A Nuclear Mushroom Cloud?

Mushroom clouds formed as a result of nuclear explosions can go thousands of meters in the sky, easily surpassing the height of Mt. Everest – the tallest mountain peak in the world.

The strength of nuclear explosions is measured in Kilotons and Megatons of TNT. The TNT equivalent is generally used to express the amount of energy released in a bomb’s explosion. A bomb is marked to have a yield of ‘1 Kiloton’ when its detonation releases a certain amount of energy which is equivalent to detonating 1,000 kilograms of TNT.  1 Megaton is equivalent to 1,000 Kilotons.

The nuclear explosion that occurred in Hiroshima, Japan in 1945 exploded with an energy of 15 kilotons.

hiroshima atomic bomb
Mushroom cloud from the atomic bombing of Nagasaki, Japan on August 9, 1945. Fireballs caused by explosions rise very quickly through the air. (Image Source: Wikimedia Commons)

What Are The Biggest Nuclear Bomb Explosions Of All Time?

These are the 3 most powerful man-made explosions in the history of mankind (in descending order of their strength):

  1. The biggest, most powerful nuclear explosion of all time occurred as a result of the detonation of Tsar Bomba, the most forceful nuclear weapon ever detonated. It was a Soviet bomb tested on 30 October 1961 over Novaya Zemlya, with a yield of about 50 megatons - around 3,300 times the energy of the Hiroshima explosion. (Its original design called for 100 Mt, but it was fielded with a lead tamper instead of uranium to roughly halve the yield and the fallout.)
  2. The second-most-powerful nuclear weapon ever fielded was the American B-41, a thermonuclear bomb deployed in the early 1960s with a design yield of about 25 megatons - though, unlike Tsar Bomba, it was never tested at full yield.
  3. Among test detonations, the next-largest after Tsar Bomba was the Soviet Test 219 on Novaya Zemlya in 1962 at about 24 megatons. The largest American test was Castle Bravo, fired in March 1954 with a yield of around 15 megatons - more than twice what its designers had expected.
nuclear explosions in history
A comparison of some of the biggest nuclear explosions till date

As you can see, a sudden, rapid and concentrated release of heat in a relatively cool surrounding is all it takes to form a mushroom cloud in the sky. So, the next time you see an image of a mushroom cloud, don’t jump to the ‘it must be nuclear way’ conclusion; it might just be a powerful volcanic eruption or a raging forest inferno. Neither of those options are ideal either, but it’s better than a sign that the nuclear apocalypse has begun!

References (click to expand)
  1. Mushroom cloud - Wikipedia. Wikipedia
  2. Rayleigh–Taylor instability - Wikipedia. Wikipedia
  3. Mushroom Cloud Physics: Not Just for Nukes. Popular Mechanics