Symmetry of Snowflakes
surface bump...................dendrite ...........complex snowflake
One thing you notice right away about snow crystals is that
they form some elaborate and complex shapes -- often displaying
lacy, branching structures. Where does this complexity come
from? After all, snow crystals are nothing more than ice
which has condensed from water vapor. How does the simple
act of water vapor freezing into ice produce such intricate
The answers to these questions lie in just how water molecules travel through the air to condense onto a growing snow crystal. The water molecules have to diffuse through the air to reach the crystal, and this diffusion slows their growth. The farther water molecules have to diffuse through the air, the longer it takes them to reach the growing crystal.
So consider a flat ice surface that is growing in the air. If a small bump happens to appear on the surface, then the bump sticks out a bit farther than the rest of the crystal. This means water molecules from afar can reach the bump a bit quicker than they can reach the rest of the crystal, because they don't have to diffuse quite as far.
With more water molecules reaching the bump, the bump grows faster. In a short time, the bump sticks out even farther than it did before, and so it grows even faster. We call this a branching instability -- small bumps develop into large branches, and bumps on the branches become sidebranches. Complexity is born. This instability is a major player in producing the complex shapes of snow crystals.And since the ambient atmospheric conditions are nearly identical across the crystal, all six budding arms grow at roughly the same rate.
The temperature seen by the snow crystal is not constant in time, however, since the crystal is being blown about and is thus carried over great distances in a cloud. But the crystal growth rates depend strongly on temperature. Thus the six arms of the snow crystals each change their growth with time, reflecting the ever-changing conditions in the cloud. And because each arm sees the same conditions, each arms grows the same way.
When the branching instability applies itself over and over again to a growing snow crystal, the result is called an ice dendrite. The word dendrite means "tree-like," and stellar dendrite snow crystals are common.
We can change diffusion in the lab and see how dendrites change. If one grows snow crystals in air below atmospheric pressure, they have fewer branches. This is because diffusion doesn't limit the growth so much at lower air pressures, so the branching instability is not so strong. At higher pressures, more branches appear.
The growth of snow crystals depends on a balance between faceting and branching. Faceting tends to make simple flat surfaces, while branching tends to make more complex structures. The interplay between faceting and branching is a delicate one, depending strongly on things like temperature and humidity. This means snow crystals can grow in many different ways, resulting in the great diversity we see in snow crystal forms.
So that's the story. It may take an online MBA or to be a master at geographic information technology to fully understand this process to the exact science of it but it is a little simpler than it seems. Having a MBA or being a master of the geographic world will definitely help in understand the fine details, but they are not necessary to see that there is something going on here. The intricate shape of a single arm is determined by the ever-changing conditions experienced by the crystal as it falls. Because each arm experiences the same conditions, however, the arms tend to look alike. The end result is a large-scale, complex, six-fold symmetric snow crystal. And since snow crystals all follow slightly different paths through the clouds, individual crystals all tend to all look different.