Globs Of Cold Air And Waves

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Last time in weather school we started to examine why our particular part of the world has such changeable weather. We looked at general global circulation patterns and then examined the zone where the westerly winds bump up against the easterly polar winds, creating giant eddies of swirling air.

This time we are going to continue our look at these swirling eddies of air and tie in something that is known as Rossby Waves, named after the meteorologist Carl Rossby, who in 1938 mathematically described how the boundary between the cold Arctic air and the milder air to the south interact.

One way to think about Rossby waves is to picture the cold air over the poles or top of our planet as a big glob of goo. If you dropped a pile of goo on top of a ball it would want to sag. The same holds true for the cold air in the Polar Regions – it wants to sag to the south. Now, things would be pretty straightforward if this was all we had to worry about, but as we all know, this simple picture is missing one important part, our planet is not just a ball simply sitting in place – it is spinning.

This spinning motion takes the atmosphere along with it, so our pile of cold air, or goo, is spinning around. So now we have a spinning pile of cold air at the top of our planet that is trying to sag towards the south. This sagging creates undulations or waves along the boundary of this cold air and it is these waves that we call Rossby waves. One of the best ways to understand this is with a diagram. If you look at the diagram I have included with this article you will see the development of a Rossby wave in three steps.

In the first image we can see that there are some slight undulations along the boundary between the cold and warm air. Over time these undulations become larger waves like we see in the second image. These waves are beginning to develop into eddies, and are becoming areas of low pressure. In the final image we see a very strong Rossby wave pattern where one of the eddies of cold air, or areas of low pressure, is starting to break away from the main area of cold air. When this happens we get what is called a closed upper low, and these can sit over an area and slowly spin down over a fairly long time, bringing with them cool, cloudy and generally miserable weather; but more on that in a future article.

At any given time there will typically be between four and six Rossby waves at different stages of development in the northern hemisphere. In our next lesson we will continue to focus in on what causes our weather because, believe it or not, it is much more complicated than simply watching out for Rossby Waves.

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