"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."
|What exactly is an ice crystal?|
A crystal is a material for which the molecules inside are all lined up in a specific way called the crystal lattice. The water molecules in ice form a hexagonal lattice as shown at right (two views of the same thing). Each red ball represents an oxygen atom, and the grey sticks represent hydrogen atoms. There are two hydrogens for each oxygen, making the usual H2O.
|Why do snow crystals form in such complex symmetrical shapes?|
answer this question in several parts. First,
Why are snow crystals six-fold symmetric?
The hexagonal symmetry of snowflakes originates with the underlying symmetry of the ice crystal lattice. Water molecules hook up in a hexagonal lattice (see the Snowflake Primer), and the molecular symmetry is imparted to the snow crystal form via faceting (see Crystal Faceting for more on how this works).
In particular, tiny snow crystals are usually in the form of small hexagonal prisms (see the Snowflake Primer), which is how the six-fold symmetry of snowflakes gets its start.
Second, let's ask
Finally, let's look at the original question by
following the life story of a complex symmetrical snow crystal.
Click on image to view.
| When water freezes into ice, the
water molecules stack together to form a regular crystalline lattice, and
the ice lattice has six-fold symmetry (see the
Primer). It is this hexagonal crystal symmetry that ultimately
determines the symmetry of snow crystals.
But then one must ask how molecular forces, which operate at the molecular scale to produce the crystal lattice, can control the shape of a snow crystal some ten million times larger. The answer to this has to do with how crystals form facets.
Facets appear on many growing crystals because some surfaces grow much more slowly than others. If we imagine beginning with a small round ice crystal, then mostly we would find that the surface was quite rough on a molecular scale, with lots of dangling chemical bonds. Water molecules from the air can readily attach to these rough surfaces, which thus grow relatively quickly. The facet planes are special, however, in that they tend to be smoother on a molecular scale, with fewer dangling bonds. Water molecules cannot so easily attach to these smooth surfaces, and hence the facet surfaces advance more slowly. After all the rough surfaces have grown out, what remains are the slow-moving facet surfaces. The picture at right shows the idea for a crystal with four-fold symmetry (which is easier to draw).
Faceting in snow crystals produces hexagonal prisms like the ones at left, which are the simplest form of snow crystals. These specimens were collected at the South Pole by Walter Tape (see Photos), where the crystals grow very slowly, allowing the facets to fully develop.
|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 designs?|
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
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.
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 (see the
Guide to Snowflakes).
The growth of snow crystals depends on a balance between faceting (see Crystal 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.