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Lightning is a huge electric spark that jumps between clouds or toward the ground.

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The longer version

Inside a storm cloud, collisions between ice crystals and soft hail separate electric charge, leaving one region positive and another negative. When the difference grows large enough, the air breaks down as an insulator, a conducting channel forms, and the stored energy is released in a fraction of a second.

That discharge is what we see as a flash. It may jump between oppositely charged parts of the cloud, between two clouds, or down toward the ground. The channel suddenly heats the surrounding air, and the violent expansion that follows produces the shock wave we hear.

Where this entry sits

Clouds, wind, rain, and storms shape daily life in ways that most people barely notice. This collection explains snow, lightning, rainbows, the turning seasons, temperature, the instruments forecasters rely on, and scraps of old weather lore. The full list sits on the Weather and Climate page, where every entry is listed in order.

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23

Thunder is the sound of air expanding rapidly after lightning heats it to extreme temperatures.

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The gap between a flash and its thunder gives a rough sense of distance.

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A rainbow appears in the part of the sky directly opposite the sun.

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Halos around the sun or moon come from light passing through tiny ice crystals.

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Red sunsets happen because sunlight travels through more air and loses its blue wavelengths.

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Seasons happen because Earth's axis is tilted, not because of distance from the sun.

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Summer days feel hotter because sunlight strikes the ground at a steeper angle.

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