Even in summer it’s cold up there — and that’s good

This map shows the amount of precipitation that has fallen across the Prairies so far this growing season as a percentile. The wettest region is around Edmonton, with precipitation amounts falling into the 90th to 100th percentiles. The driest areas are in southern Alberta and central Manitoba, with some areas seeing values as low as the 10th to 
20th percentiles.
Reading Time: 4 minutes

Last issue, we looked at how precipitation forms in warm clouds.

But in reality, most of our summertime precipitation comes from thunderstorms, which primarily consist of cold clouds, so we’ll take a look at what cold clouds are and how precipitation forms in them.

In general, a cold cloud is one that has at least some part of it that is below the freezing point. In Alberta, this cloud dominates the weather for most of the year, even in the summer.

Before we look at the precipitation process in cold clouds, we need to explore the idea of super-cooled water. All of us at some point have experienced freezing rain. Most occurrences of freezing rain occur when temperatures are just slightly below zero. This means that the surfaces the raindrops are falling on and freezing to are just a little below zero.

Now, if you have ever dropped some cold water onto a freezing surface you would notice that the water does not freeze instantaneously (unless the surface is very cold). So, why then, does the raindrop falling from the sky freeze as soon as it hits a solid surface? Because that falling raindrop was super cooled — the liquid water in the raindrop is actually below the freezing point.

How is this possible?

We’ve all learned that water behaves differently than most other substances on earth. While other substances are most dense when they become solid, water is most dense at 4 C. (If water didn’t behave in this way we wouldn’t be here. Just think what would happen to rivers, lakes and oceans if ice were heavier than water.)

And the uniqueness of water doesn’t end there. Strangely enough, when we are looking at water in the atmosphere it doesn’t normally freeze at 0 C.

Just as water droplets need something to condense onto in order to freeze, ice crystals need something to freeze onto. The problem that arises is that in the atmosphere there are large numbers of particles for water to condense onto (condensation nuclei), but very few particles for water to freeze onto (ice nuclei).

For ice to form (at temperatures just below zero) you need a six-sided structure, and there are not many of these around. Ice crystals themselves are six sided, but where do you get the ice crystal in the first place?

Because of this, if the cloud temperature is warmer than -4 C, the cloud will be made up of super-cooled water. If we cool the cloud down to around -10 C, ice crystals will begin to form even if there are no ice nuclei, so at these temperatures the cloud will consist of a mixture of ice crystals and super-cooled water. Once temperatures fall to -30 C the cloud will consist almost entirely of ice crystals, and if we are colder then -40 C the entire cloud will be made up of ice crystals.

OK, so now we know that within cold clouds we will usually have a combination of ice crystals and super-cooled water, this is Step 1 in our process of creating precipitation in cold clouds. On to Step 2: the Bergeron Process.

The Bergeron Process relies on another unique property of water, and that is, if there is just enough water vapour in the air to keep a super-cooled water droplet from evaporating, then there is more than enough water vapour in the air for an ice crystal to grow larger. Because the saturation vapour pressure over ice is lower than that over water, ice crystals will attract water vapour more readily than water droplets will.

Our cold cloud now has ice crystals in it and these ice crystals are growing. As the crystals grow they pull water vapour from the atmosphere. As the amount of water vapour in the atmosphere drops, our super-cooled droplets will begin to evaporate to help make up the difference. These droplets evaporate and the ice crystals continue to grow at the expense of the super-cooled water droplets. After a while, the cloud consists mostly of ice crystals.

This process by itself would only result in light amounts of precipitation though, for heavier precipitation we need a third process to kick in. In a cold cloud we call this third process riming and aggregation.

If you recall, in warm clouds rain develops through a process known as collision and coalescence, where water droplets collide and grow together until they are big enough to fall to the ground. In a cold cloud we call a similar process riming and aggregation and it produces a similar result — ice crystals large enough to fall to the ground.

Within cold clouds, ice crystals fall and collide into either super-cooled water and grow larger (riming), or they collide into other ice crystals and grow larger (aggregation). Aggregation occurs best when cloud temperatures are only slightly below zero, as the warmer temperatures allow the ice crystals to have a wet surface which helps other ice crystals stick to them.

This is one of the reasons we see large snowflakes when it is relatively warm.  Of course, in the summer, when our lower atmosphere and surface temperatures are warm/hot, the ice crystals melt on the way down and fall as rain. As you can see, most of our precipitation, even in summer, comes from cold clouds courtesy of the Bergeron Process and the processes of riming and aggregation.

In the next issue we’ll continue our look at clouds by examining the different types of clouds and how they are named and classified.

About the author

AF Contributor

Daniel Bezte

Daniel Bezte is a teacher by profession with a BA (Hon.) in geography, specializing in climatology, from the University of Winnipeg. He operates a computerized weather station near Birds Hill Park, Manitoba.



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