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It starts with the gathering of clouds into a storm. In the center of the growing storm, tiny flecks of ice and supercooled water droplets collide and exchange charge, with positive charge billowing into the storm’s spreading anvil. The flow of particles creates an imbalance; the system needs to neutralize. Finally, with a zap having more power than 100,000 radio stations, all concentrated at a single point, lightning strikes.
As a journalist, you can create a free Muck Rack account to customize your profile, list your contact preferences, and upload a portfolio of your best work.
