To become active thunderstorms, parcels of lifted, saturated air must keep rising - spurred by the latent heat released by condensation.
Eventually the warm air hits the ever-present inversion layer at the top of the troposphere, 9km to 12km above land. The top of the cloud is then forced to spread laterally.
Lightning erupts in the freezing heights of the troposphere as super-cooled water droplets collide with ice crystals, building up static electricity.
A narrow channel of air is superheated as lightning passes through, expanding and rumbling as thunder.
"It's not often you get to watch the complete cycle of wild weather evolving from beginning to end," Dr Revell said. "A summer thunderstorm is natural theatre on a grand and spectacular scale."
Forecast
Auckland
Today: Long fine spells. Northwest breezes developing.
Tomorrow: Fine and cloudy periods. Northwesterlies.
Thursday: Rain developing, some heavy falls. Northwesterlies.
Hamilton
Today: Long fine spells. Northwest breezes developing.
Tomorrow: Cloudy periods. Northwesterlies.
Thursday: Rain developing, some heavy falls. Northwesterlies.
Wellington
Today: Becoming cloudy, some drizzle. Gale northerly.
Tomorrow: Drizzle turns to rain later. Gale northerly.
Thursday: Rain, sometimes heavy, eases to showers. Northerly eases.