Snow, sleet, freezing rain and hail: What's the difference?

Depending on the journey through the atmosphere, it could be snow, hail, sleet, or freezing rain falling from the sky. Three of those require winter storm ingredients but hail can happen any time of year.

A storm has passed through, and the ground is covered in frozen precipitation, which, depending on its journey through the atmosphere, could be snow, hail, sleet, or freezing rain.

Three of the four listed require winter storm conditions, but one can happen year-round—even in the summer.

What makes Snow?

Snow is the most common, of course. Snowflakes form when water vapor freezes directly to ice while skipping the part of being a raindrop first. 

"Snowflakes that most of us are used to seeing are not individual snow crystals but are actually aggregates, or collections, of snow crystals that stick or otherwise attach to each other," according to NOAA. "Aggregates can grow to very large sizes compared to individual snow crystals."

7 FACTS ABOUT SNOW

Precipitation remains snow as long as the air mass stays below freezing throughout the snowflake's journey from cloud to ground.

It begins to snow between 18,000 and 25,000 feet in the upper atmosphere, and the precipitation changes based on the air it encounters. If the air remains below 32 degrees, it will fall to the ground as snow. 

HOW COLD DOES IT HAVE TO BE TO SNOW?

If warmer air starts to intrude into the region, then things get dicey.

How do freezing rain and sleet form?

Both sleet and freezing rain start with a snowflake that melts into a raindrop as it encounters a slice of warmer air on its free-fall through the atmosphere. But if there is a renewed area of freezing temperatures near the ground, the drop will refreeze. 

WHAT IS FREEZING RAIN?

If the wedge of warm air is relatively narrow and the area of freezing air is fairly thick, the raindrop will have time to freeze back into an ice pellet. This is known as sleet (or on weather observations as "ice pellets" or "P").

WHAT IS AN ICE STORM?

Sleet can accumulate on the ground, but it is like stepping on zillions of tiny frozen raindrops.

Freezing rain comes when the wedge of warm air is relatively thick, and the area of freezing air hugging the ground is shallow. In this case, the raindrop doesn't have quite enough time to freeze into a solid but instead becomes "supercooled" to the cusp of freezing. 

WHAT TO KNOW ABOUT ICE STORMS

Once it hits the surface, it will instantly freeze to wherever it landed. 

This process will result in freezing rain, or part of an "ice storm," and can be the most dangerous frozen precipitation. If you ever see a weather observation with the code "ZR," it's short for "freezing rain."

Unlike sleet, which is more of an accumulation of pellets, freezing rain creates an icy glaze and turns streets and sidewalks into increasingly-thick sheets of ice, making driving and walking quite treacherous.

What's worse, the ice is transparent, and many unsuspecting drivers can find themselves hurtling forward with no traction and no way to control their vehicle if they suddenly reach a road that was just hit by a freezing rain event. 

Some of America's worst crashes, involving dozens to hundreds of cars, have happened in freezing rain events.

HOW MUCH ICE IS NEEDED TO KNOCK OUT POWER, DAMAGE TREES?

Freezing rain will also coat tree branches and power lines, and if enough weight accumulates, it can topple them both, leading to widespread power outages and tree damage.

Simply put: Freezing rain and ice storms are a mess and require extreme caution during these events. 

What makes hail?

Hail is the one frozen precipitation that can fall no matter the date on the calendar or the temperature outside. 

Hail refers to balls of ice that can range from the size of a pea to a volleyball, and fall from a cumulonimbus (thunderstorm) cloud. 

Hailstones’ sizes are dependent on the strength of the storm's updraft

WHAT CAUSES DIFFERENCES IN HAIL SIZE?

A raindrop freezes into an ice pellet and then falls, picking up raindrops through warmer sections of the cloud until it hits the updraft and gets blown skyward where that extra water freezes, making the hail larger and heavier before it falls again.

The process repeats until the hailstone is heavier than the updraft can support, and then it falls to the ground. 

 7 THINGS TO KNOW ABOUT HAIL

Updrafts of 50-plus mph can create huge hailstones that are golf ball, baseball-sized or even "gargantuan"-sized.

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