Why does hail fall in summer, the hottest time of year?

Snow comes when it's freezing — that makes sense. But the biggest chunks of solid ice fall on hot, sticky summer afternoons. How does a sweltering day make ice the size of a marble? Let's climb inside a storm cloud and find out.

1Two things hiding inside a storm cloud

It's freezing up top — and the hot ground makes a rising wind

You only need two ideas. Watch each one:

The cloud-top is freezing

A tall storm cloud is warm and sticky down low, but far below freezing up high. Even on a hot day, the very top of the cloud is colder than your freezer.

Hot ground makes air rise

Sun-baked ground heats the air, and warm air shoots upward. That rising column is an updraft — an invisible wind blowing straight up the middle of the cloud.

2Two kinds of updraft

A gentle puff vs a violent blast

Not every storm has the same upward wind. The whole story turns on how strong that updraft is:

Weak updraft

The gentle puff

A soft breeze of rising air. An ice pellet drifts down through it and falls out the bottom.

Strong updraft

The violent blast

A fierce column of rising air, strong enough to catch a falling pellet and shove it back up.

3Your turn — be the storm's wind

Drag the updraft and feel it push on a pellet

Here's one little ice pellet floating in the cloud. Slide the updraft from a puff to a blast and watch how hard the rising wind pushes back on it — a strong updraft can hold it up high; a weak one lets it sink.

Updraft strength: a gentle puff
WEAK PUFFVIOLENT BLAST

4Now grow a real hailstone

Drop a pellet in and watch it try to grow 🧊

Here's the test. A pellet only grows by looping up to the freezing top, picking up a frozen coat, falling, and getting caught and flung up again — a new layer every loop. Same pellet, two storms. Guess first, then release it.

Guess before you release it

What makes a hailstone grow big — a weak updraft, or a strong one?