How does it work? (The Quick Explanation):
The science of snowmaking can be quite complex. For the majority of us, however, a simple explanation of how the different parts of a snowmaker act will suffice. Snowmaking in its simplest form is the act of turning water into small ice crystals (snow). In order to make snow from your home water supply (at about 50°F), it must be cooled very rapidly. Four things come into play to make this happen: ambient temperatures, evaporation, surface area, super cooling.
Ambient Temperature
First it must be cold outside. Even when the outdoor temperature is below freezing (32°F) snow quality can be poor or slushy. This is because much of the water is not staying or even turning into the frozen state. If you refer to our snowmaking weather chart, you will see what the ideal temperatures are for snow making.
Evaporation
The second factor is heat loss through evaporation. As some of the water evaporates from the surface of the drop a small amount of heat is removed from the drop itself. Try putting some rubbing alcohol on your arm. As it evaporates you will experience this cooling effect. Your body uses this process of evaporation to cool itself, we call it sweating. When the air is humid, there is already a lot of moisture in the air. Your sweat is less readily absorbed into the air and is unable to evaporate from your skin removing the heat with it. The same premise happens in snowmaking. When there is high humidity, the water droplet’s surface is not able to evaporate a small amount of water and remove some of the heat. Therefore, in snowmaking we must refer to the “Wet Bulb Temperature”. This is a measure of the ambient temperature that takes into account the cooling effect the humidity in the air allows for.
Surface Area
The third way we cool the water is by increasing the surface area of the drop. By increasing the surface area, we expose as much of the water to the cold as possible. The smaller we make these drops,(4500 psi pushed thru a .009 orfice ) the greater the surface area to volume ratio. We achieve the proper drop size and spray pattern through our highly specialized nozzles. And yes, the nozzles do matter! In order to optimize the size of the droplets, the distance between the drops, and the water volume flowing though the opening while employing high pressures to achieve proper distance and hang time, we engineered nozzles specifically for snowmaking.
Super Cooling
Finally we need to look at super cooling. When a compressed gas (in this case air) is allowed to rapidly expand, there is a decrease in temperature. This is known as the Joule-Thomson Effect. The conditions at the air nozzle are such that the mist coming from the nucleation nozzle is able to immediately freeze. These tiny ice crystals are then drafted into the larger upper mists which seed and snap the pre-cooled water droplets into a frozen state. The result is snow that then falls out of the mist.
Here is a site :arrow: I wish this site had been around 10 years ago. :wink:
Video http://www.youtube.com/watch?v=I3mnsmXyvqA
http://www.snowathome.com/snowmaking_science.php