Water vapor form snowflakes when the temperatures in the air are above freezing and the air should be unsaturated. The water vapor to create hailstones start inside a cumulonimbus cloud and super cooled liquid water are caught in a strong updraft. The cycle continues to increase the size of the hailstone, then eventually falls to the earth's surface.
The snowflakes getting Bigger.
Inside any cloud water is constantly evaporating an recondensing in an equilibrium that maintains the cloud and keeps the droplets too small to fall to the ground. One ice crystals form, however the equilibrium shifts toward ice. Water vapor in the colder parts of the cloud will tend to freeze rather than condense, forming snowflakes which begin to fall. When it snows, these flakes simply fall to the ground, sometimes coalescing. For rain, the snowflake melt and become raindrops.
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It is compacted and cemented by minerals.
Mountain Ranges form. Like the Himalayas
The snowflakes getting Bigger.
The snowflakes fly across the screen during the winter fest and if you click on them you will get a gift. the winter fest happens during Decmber or January. Hope this helps!
they fall toward the ground. by khulood
The crystalization process that forms snowflakes happens randomly, and the number of different ways that a snowflake can form is very large, so it is improbable that any two will be alike.
She interviews celebrities and people who have interesting stories.
You dont have snow flakes at degrees above 0, because then it is not snow, but rain
In rocks large crystals form from very SLOW cooling.
It is called hailstones or ice.
Snowflakes are star-shaped due to the molecular structure of water and how it freezes. When water freezes, water molecules arrange themselves in a hexagonal lattice, forming a six-sided structure. As more water molecules freeze and accumulate, the lattice grows and gives snowflakes their characteristic star shape with six branches. The intricate patterns and variations in snowflake shapes occur due to the unique environmental conditions and the individual paths water molecules follow as they freeze in the atmosphere.
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No
Inside any cloud water is constantly evaporating an recondensing in an equilibrium that maintains the cloud and keeps the droplets too small to fall to the ground. One ice crystals form, however the equilibrium shifts toward ice. Water vapor in the colder parts of the cloud will tend to freeze rather than condense, forming snowflakes which begin to fall. When it snows, these flakes simply fall to the ground, sometimes coalescing. For rain, the snowflake melt and become raindrops.