What would it feel like to touch a cloud?
They may look comfy to sit on but you’d plummet through and hit the ground.
You might already know how it feels to touch a cloud without realizing it.
If you’ve ever been outside on a foggy day, you’ve essentially been inside a cloud, just one very close to the ground instead of high in the sky. Fog and clouds are both made of tiny water droplets – like the ones you can sometimes see or feel in a hot, steamy shower.
Clouds form through evaporation and condensation. Water in lakes, rivers, oceans, or puddles evaporates into water vapor as the sun heats it up. You can evaporate water yourself by boiling it – watch it disappear like vapor.
Water vapor, which is invisible, naturally rises up from the Earth’s surface into the atmosphere as warm bubbles, like the bubbles you’d see rising in a lava lamp. The higher it goes, the more it cools, until eventually, the water vapor condenses back into liquid water.
Clouds are made of millions of these tiny liquid water droplets. The droplets scatter the colors of the sunlight equally, which makes clouds appear white. Even though they can look like cushy puffballs, a cloud can’t support your weight or hold anything up but itself.
Water vapor in your bathroom can fog up the mirror.
The process of evaporation and condensation in the atmosphere is similar to what happens in your bathroom when you take a hot shower: Warm water evaporates and then condenses back into the water on the cold mirror.
Water vapor does not condense spontaneously. It needs tiny particles or a surface – like your bathroom mirror – on which to form a drop. Atmospheric scientists like me call these tiny particles cloud condensation nuclei or CCN for short. These CCN are just dirt or dust particles that have been lifted by the wind and are floating around in the atmosphere.
Does that mean that places with a lot of dust and pollution, like cities, have more drops than clean places? Researchers have found more tiny droplets and more clouds in areas where there are a lot of these cloud condensation nuclei, while in areas without them fewer clouds are observed, like over the ocean or the Arctic.
Water evaporates and rises up into the sky, condensing to form clouds.
As cloud droplets rise in the atmosphere, the air temperature decreases. The tiny cloud droplets start to freeze when the temperature drops below 32 degrees Fahrenheit (0 degrees Celsius). It’s the exact same process as making ice cubes in a freezer.
The frozen droplets are now ice crystals. They continue to grow in size as water vapor turns into ice and sticks onto them. Scientists call this process of a gas turning into a solid “deposition.” It creates the beautiful branched ice crystals that you find in snowstorms.
Those spiky arms can grab on to other snowflakes.
Steady updrafts of air keep these very light water droplets or ice crystals floating in the cloud. So how do they turn into rain and snow and fall to the ground? Easy, they join forces.
Larger droplets collect smaller droplets on their way to the ground as raindrops. Snow grows in a similar way, with the crystals sticking to each other. Their little arms can interlock to form a bigger snowflake. When water droplets merge with ice crystals, that makes hail.
Rain droplets grow on their way down to the ground, eventually becoming unstable and breaking up. The largest raindrop that researchers have found was about a third of an inch across. Some giant snowflakes have been reported to be as big as 6 inches across. And the biggest piece of hail? In 2010, someone found a hailstone 8 inches in diameter in South Dakota and took a photo – so scientists know it was real.
That would be a lot more painful to collide with than a wispy cloud of water vapor.
This article was originally published on The Conversation by Katja Friedrich at the University of Colorado Boulder. Read the original article here.
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