Snow in Different Languages: Snow are small particles of ice that grow in cold atmosphere. They are dispersed in the clouds and then fall in very cold temperature. Snow constitutes frozen crystals of water for the whole of its life cycle, emerging with ice crystals forming in the atmosphere under appropriate conditions, rising to millimeter level, precipitating and accumulating on surfaces, metamorphosing in place, and finally freezing, sliding or sublimating away.
How to Say Snow in 88 Different Languages
|Different Languages||Word Snow|
|Chinese Simplified||雪 (xuě)|
|Chinese Traditional||雪 (xuě)|
Snowflakes cluster around atmospheric particles by attracting super cool water droplets that form into hexagonal crystals. Snowflakes assume a variety of forms. The polar regions, northernmost part of the Northern Hemisphere, and mountain regions around the world, are large-scale ice-prone, because of cold temperatures and humidity. Ice is mainly restricted to mountain regions outside the Antarctica in the Southern Hemisphere.
Snow affects human activities including transportation such as the need to keep roads, wings and windows clear; in agriculture to provide crops with water and animal welfare; snow effects warfare. Snow also affects ecosystems by providing a layer of insulation in the winter in which plants and animals can survive the cold.
It can also be classified as a mineral because snow is made up of frozen water or ice. A mineral is an inorganically created, uniform solid with an orderly atomic structure and a definite chemical composition. Ice occurs naturally, with temperatures below 0 degrees Celsius (32 degrees F). It is homogeneous, formed inorganically (of one material), and has an ordered atomic structure. Ice has a clear chemical composition (H20), with unique bonding of hydrogen and oxygen atoms.
Snow supports a wide range of animals on and below the surface. Many invertebrates, including spiders, wasps, beetles, snow scorpionflys and springtails, thrive in snow. Typically, such arthropods are active at temperatures below -5 ° C (23 ° F).
When you look at a snowflake under a microscope, you can see that every crystal has a beautiful, symmetrical six-spoken form. No two snowflakes are ever same. Every snowflake has a different structure and have millions of shapes.