Precipitation Forming Processes

An error occurred trying to load this video.

Try refreshing the page, or contact customer support.

Coming up next: Global Precipitation Distribution's Relation to Wind & Pressure Patterns

You're on a roll. Keep up the good work!

Take Quiz Watch Next Lesson
 Replay
Your next lesson will play in 10 seconds
  • 0:02 What Is Precipitation?
  • 2:28 Growth in Warm Clouds
  • 3:22 Growth in Cool and Cold Clouds
  • 5:18 Lesson Summary
Save Save Save

Want to watch this again later?

Log in or sign up to add this lesson to a Custom Course.

Log in or Sign up

Timeline
Autoplay
Autoplay
Speed Speed
Lesson Transcript
Instructor: Elizabeth (Nikki) Wyman

Nikki has a master's degree in teaching chemistry and has taught high school chemistry, biology and astronomy.

In this lesson, you will learn how water molecules turn into precipitation. Also, you will discover how varying conditions can lead to different types of precipitation.

What Is Precipitation?

It's a gorgeous sunny day, and you've just settled down by the pool. There's not a cloud in the bright blue sky, when suddenly the sky grows a bit darker. You look up to see a cloud blocking the sun! Not only that, you hear the rumbling of thunder. As the pitter patter of rain begins, you are forced to go inside.

Rain is a form of precipitation, or water that falls from the sky to the surface of the earth. Precipitation may be in liquid form, like rain, or in solid form, like snow. It's easy to get disgruntled by rain or snow on a day when you'd rather be outside getting some sunshine. But the phenomenon of precipitation is actually quite cool--literally!

To better understand how precipitation forms, let's imagine that we are up in the atmosphere and only about 10 micrometers large. Just in case you don't remember, one micrometer is one one-thousandth of a millimeter. Though you may not see them, you are surrounded by countess gaseous water molecules, known as water vapor. When the air becomes saturated with water vapor, meaning there is more water vapor than the air can hold, clouds will form. This usually happens at high altitudes, but it can happen at lower altitudes. Ever been in a fog?

The state of being saturated is similar to being in a really crowded room; every available space is occupied. Once the room is too crowded, you and other people might be forced to leave. In the case of cloud formation, water vapor is forced to condense into water droplets or ice crystals. Collectively, all these droplets and ice crystals make up a cloud.

A cloud is a region of atmosphere where moisture condenses, forming tiny water droplets or grains of ice. As you're looking around, you see water droplets that range from one to ten times your size. All of the droplets inside the rain cloud are falling, but movement is so slow that air currents are strong enough to push them back up. In our cloud, we can also see small grains of ice. Their individual shapes vary; however, all bear semblance to a hexagonal structure.

Water vapor molecules have condensed onto condensation nuclei, which are minuscule solid or liquid particles floating around in the atmosphere. The tiny water droplets we see collect other surrounding water molecules. This basic process is known as growth by condensation. Once the weight of the droplet is too much for the atmosphere to support it, it will fall from the sky.

Growth in Warm Clouds

Let's say we're suspended in a cloud that's warm--well, relatively warm. To be a warm cloud, temperatures just need to be above freezing. Inside our warm cloud, there are tiny water droplets. These droplets are constantly colliding with each other, and sometimes, they stick together after colliding. This process of collision and coalescence leads to the growth of rain drops.

Droplets can grow to a million times their original size through collision and coalescence! Once the drops are too big, they will fall from the cloud. On the way down, these drops will collect other droplets. If drops become too big, however, resistance from air will cause them to break down into smaller drops.

If drops pass through hot or dry air, they will evaporate before hitting the ground. If the air is above freezing, the drops will fall as rain. But, if the air is below freezing, the raindrops will freeze into sleet.

Growth in Cool and Cold Clouds

When temperatures drop below freezing, our surroundings change a bit. Inside a cool or cold cloud, both ice crystals and super cooled water can exist. Super cooled water is water that is below freezing but is still in a liquid state. Ice crystals are tiny bits of frozen water.

To unlock this lesson you must be a Study.com Member.
Create your account

Register to view this lesson

Are you a student or a teacher?

Unlock Your Education

See for yourself why 30 million people use Study.com

Become a Study.com member and start learning now.
Become a Member  Back
What teachers are saying about Study.com
Try it risk-free for 30 days

Earning College Credit

Did you know… We have over 200 college courses that prepare you to earn credit by exam that is accepted by over 1,500 colleges and universities. You can test out of the first two years of college and save thousands off your degree. Anyone can earn credit-by-exam regardless of age or education level.

To learn more, visit our Earning Credit Page

Transferring credit to the school of your choice

Not sure what college you want to attend yet? Study.com has thousands of articles about every imaginable degree, area of study and career path that can help you find the school that's right for you.

Create an account to start this course today
Try it risk-free for 30 days!
Create an account
Support