Our personalizable Christmas snowman decorations are 4½ inches tall. The Christmas snowman decorations are a snowy looking Christmas stocking with a white cuff that looks like melting snow. Just below the cuff on the snowman ornaments there is a Christmas red space and then the toe of the stocking is snowy white. In the center of the Christmas ornament is a small snowman wearing a blue and red Santa hat and a blue and white striped scarf. The little snowman has pink cheeks, a pink nose, black buttons and brown stick arms. Behind the little snowman is a decorated Christmas tree. On the toe of the snowman stocking ornament is a small blue, red and white candy train. The cuff of the personalizable Christmas snowman decorations is 2 inches long and ¾ of an inch wide and is perfect for adding the name of someone very special. The personalizable snowman decorations hang from a red cord.
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Amounts of Snowfall.
Snowfall varies greatly across the earth. Snow falls in the Polar Regions throughout the year. The heaviest snows occur during the winter in mountainous areas of the temperate zones, between the Tropic of Cancer and the Arctic Circle and between the Tropic of Capricorn and the Antarctic Circle. These areas include the western coastal ranges of North and South America and the Alps in Europe.
In the United States, the record for snowfall in one year was set from July 1971 to June 1972 when 1,122 inches of snow fell at Rainier Paradise Ranger Station in Washington. In 1921, 76 inches of snow fell in silver Lake, Colorado, which set a record for the largest snowfall during a 24 hour period.
A typical layer of snow on the ground would melt to form a layer of liquid water about one tenth as thick as the snow. One inch of water may be equivalent to as much as 30 inches of dry, fluffy snow. Snow is a major source of water in many places Mountain snowmelt, for example, feeds many rivers and streams.
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How Snow Forms.
Snow crystals usually start from tiny droplets of super cooled water. Water droplets do not always freeze at the normal freezing temperature of water, 32 degrees F. Droplets of super cooled water remain liquid even though their temperature is below the freezing point.
At the beginning of the process of snow formation, some super cooled droplets freeze. They do so because they contain or come into contact with tiny particles called freezing nuclei or ice nuclei. Most freezing nuclei are dust or specks of plant debris raised by the wind.
Nearby, water droplets, which are still super cooled, slowly evaporate. Much of the resulting vapor joins the crystals and so the crystals grow.
The crystals fall faster and faster as they grow. They may collide with one another to make snowflakes. Snow particles fall at rates ranging from nearly zero for tiny crystals to about 3 feet per second for a typical snowflake and several times that for melting snow. Snow crystals often strike super cooled droplets, which immediately freeze onto them. This process, called riming, forms soft particles known as snow pellets or graupel. In temperate zones, the melting of snow pellets provides much of the rainfall from cumulus clouds.
Nearly all snow crystals have six sides, but they vary in shape. The crystals are six sided because the water molecules within them link together in six sided structures. Planar or flat crystals called plates range from simple hexagons to six pointed stars to the familiar finely branched dendrites. Dendrites form at a temperature of about 5 degrees F, six sided columns form at about 14 degrees F. Many columnar crystals are hollow.
Individual snowfalls usually contain many different types and combinations of crystals. Snow crystals that encounter a variety of temperatures and humidity’s as they grow may become partly planar and partly columnar. They may or may not undergo riming or clumping.
Select this link to view our Christmas tree skirts, and Christmas stockings.