Search results
Results from the WOW.Com Content Network
A mushroom cloud is a distinctive mushroom-shaped flammagenitus cloud of debris, smoke, and usually condensed water vapour resulting from a large explosion. The effect is most commonly associated with a nuclear explosion , but any sufficiently energetic detonation or deflagration will produce a similar effect.
Formation of a mushroom cloud. Depicts the drawing up of cool air into the hot cloud via the stem, and inside the cloud is a toroidal circulation of hot gases with an updraft through the center of the toroid. Outside of the center of the cloud, the gas has هتا. substantially and looks like a regular cloud.
The cumulonimbus flammagenitus cloud (CbFg), also known as the pyrocumulonimbus cloud, is a type of cumulonimbus cloud that forms above a source of heat, such as a wildfire, nuclear explosion, or volcanic eruption, [5] and may sometimes even extinguish the fire that formed it. [6] It is the most extreme manifestation of a flammagenitus cloud.
Aerial footage from the recycling plant in Oxford which was struck by lightning last night (2 October), shows the damage sustained following the incident. The explosion could be heard up to 20 ...
Nancy Baker Cahill's augmented reality public art work, which launches on Monday of Frieze Week, depicts a mushroom cloud — 'the ultimate symbol of human-caused cataclysm.'
English: For decades this image was commonly misidentified as the mushroom cloud of the Little Boy bomb that formed around 8:15 AM local time. However due to its greater height and the wholly different time of day, it is a pyrocumulus* cloud that occurs frequently over firestorms.
The observed colors of the illumination changed from purple to green and eventually to white. The roar of the shock wave took 40 seconds to reach the observers. It was felt over 100 miles (160 km) away, and the mushroom cloud reached 7.5 miles (12.1 km) in height. [108] Many observers recalled their amazement at the light from the explosion.
A transient condensation cloud, also called a Wilson cloud, is observable surrounding large explosions in humid air. When a nuclear weapon or high explosive is detonated in sufficiently humid air, the "negative phase" of the shock wave causes a rarefaction of the air surrounding the explosion but not of the air contained within it.