Atmospheric Circulation: Scale & Observation

An error occurred trying to load this video.

Try refreshing the page, or contact customer support.

Coming up next: The Single-Cell Model of General Circulation

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

Take Quiz Watch Next Lesson
Your next lesson will play in 10 seconds
  • 0:01 Atmospheric Circulation
  • 1:39 Scale & Observation
  • 4:59 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

Speed Speed

Recommended Lessons and Courses for You

Lesson Transcript
Instructor: Julie Zundel

Julie has taught high school Zoology, Biology, Physical Science and Chem Tech. She has a Bachelor of Science in Biology and a Master of Education.

Atmospheric circulation is responsible for the weather you experience. This lesson will explain how atmospheric circulation works and then it will explore how it impacts the weather in a couple of different locations.

Atmospheric Circulation

When you hear the word 'circulation', a beating heart, arteries, and veins probably comes to mind. But what about atmospheric circulation? Does the atmosphere have a giant heart with blood vessels that pumps air through the atmosphere? Of course not. But you know what? Atmospheric circulation is kind of similar to your beating heart and blood vessels with a few differences.

Instead of blood, there's air and instead of a heart that pumps blood, unequal heating of the Earth and the Earth's rotation drives atmospheric circulation. So, in a nutshell, atmospheric circulation means air traveling around the Earth due to unequal heating and the Earth's rotation. Let's take a moment to delve a little deeper into that definition, starting with unequal heating.

As the Sun's energy reaches the Earth, more heat energy reaches the Equator compared to the poles, thus creating unequal heating. The warm, equatorial air rises and heads towards the poles. As it heads north and south, however, it starts to cool, sink, and then return to the Equator. This creates a cell, or a cycle of air.

And because the Earth is rotating, the air gets deflected in what is known as the Coriolis Effect. In the Northern Hemisphere, winds are deflected to the right as they blow from high- to low-pressure systems and the opposite is true in the Southern Hemisphere where winds are deflected to the left as they blow from high- to low-pressure systems.

Now that you have a general idea of how atmospheric circulation works, let's scale down a bit so you can get a clearer picture.

Scale and Observation

The atmospheric circulation we just went over is a little more complicated than equatorial air heading to the poles and polar air heading to the Equator. There are actually several cells that occur on the Earth. For example, there is the Polar Cell that occurs near the poles, the Hadley Cell that occurs near the Equator, and the Mid-latitude Cell that occurs (you guessed it) at mid-latitudes. And in reality, it's even more complicated than that!

But let's scale down even further and see what weather someone would observe if she were living on the east coast of the United States. We'll focus on the Polar Cell in the Northern Hemisphere, but there's one in the Southern Hemisphere too!

Remember, due to unequal heating by the Sun, the North Pole has cold, dense air whereas the Equator has warm, less-dense air. The cold, dense air flows from the high-pressure system in the North Pole toward the Equator in what is known as Polar Easterly winds. And remember, the Earth is rotating, so these winds get deflected to the west. They get their name because of where they originate, at the poles and from the east.

Let's scale down a little more and take a look at these winds. They tend to be dry, cold and weak and blow from the poles to about 60 degrees latitude.

The Polar Easterlies meet up with warm, wet wind that is blowing toward the poles (or the Prevailing Westerlies) at about 60 degrees North and South latitude. The warm, wet wind from the prevailing Westerlies and the dry, cold wind from the Polar Easterlies create the polar front. A front, in case you're wondering, is just a transition between two different types of air; in this case the cold, dry air and the wet, warm air.

Now let's scale down even further to see how these winds and the polar front impact weather. On the east coast of the United States, the polar front is responsible for mid-latitude cyclones, which create blizzards and storms. In fact, in 1993, a storm occurred that was so severe it's been called the 'Storm of the Century'. This storm was one of the most expensive natural disasters during the 20th century in the United States with snow piling up from Maine to Alabama, and Florida experiencing flooding, all followed by extreme temperatures.

Let's take a moment to zoom in on another cell and see how it impacts the weather. This time, let's head closer to the Equator to look at the Hadley Cell.

To unlock this lesson you must be a 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

Become a member and start learning now.
Become a Member  Back
What teachers are saying about
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? 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