Pyrocumulonimbus cloud

About Pyrocumulonimbus clouds:

• They occur only when there is an extremely hot wildfire — volcanic eruptions can also lead to the formation of pyrocumulonimbus clouds.
• Formation
  • The intense heat from the fire warms the surrounding air which moves upward into the atmosphere.
  • As this hot and very buoyant air — carrying water vapour, smoke, and ash — rises, it expands and cools down. Once it is cool enough, water vapour condenses on ash, forming a grey or brown cloud.
  • At this stage, the cloud is known as a pyrocumulus cloud, also known as a ‘fire cloud’.
  • If there is sufficient water vapour available and the upward movement of hot air intensifies, pyrocumulus clouds can evolve into a pyrocumulonimbus cloud.
• These clouds can reach heights of 50,000 feet and generate their own systems of thunderstorms.
• Although pyrocumulonimbus clouds can produce lighting, they do not generate much rain.
• As a result, they can spark new wildfires many kilometres away from the main blaze. These clouds can also trigger strong winds that can make the spread of the wildfire faster and unpredictable.
• Scientists believe that climate change could have a role to play in the increase of their frequency.
• Studies have shown that with temperatures soaring across the world, wildfires are becoming more common and intense.