How a lightning bolt is born
Process map by Brian. 27 steps, 2 layers. Tags: science, weather, physics.
- The thundercloud: Warm, wet air surges upward into a storm cloud
- Ice crystals and soft hail: Ice crystals and soft hail collide
- The thundercloud: Cloud sorts itself: positive on top, negative at the bottom
- Ground and tall objects: The ground below turns positive, shadowing the storm
- The air (an insulator): Strong enough to break the air down?
- The bolt: The stepped leader zigzags down in 50 m jumps
- Ground and tall objects: Streamers reach up from trees, towers and people
- The bolt: Do leader and streamer meet?
- The bolt: Return stroke: the blinding flash races up at 100,000 km/s
- The air (an insulator): Air in the channel heats to 30,000 °C, hotter than the Sun's surface
- The air (an insulator): Superheated air explodes outward: thunder
- The thundercloud: Charge left in the cloud?
- The thundercloud: Storm recharges, or fades away
- The bolt: Leader branches and searches for another path
- The thundercloud: Collisions keep piling up charge