How is the rime in Huangshan Mountain formed?

Rime has two main shapes. One is that supercooled water droplets quickly freeze into small ice cubes after hitting cold ground objects, which is called particle rime (or hard rime) and has a relatively compact structure. The other is the crystalline rime (or soft rime) formed by the condensation of water vapor generated when water droplets evaporate, which has a loose structure and will fall off with a slight vibration.

Rime is a kind of white or milky opaque ice layer attached to the windward surface of ground objects (such as branches and wires). Because there are many gaps between water droplets in the rime, the rime is completely opaque white. The rime is pale and white, attached to trees and objects, just like a silver flower of a tree, delicate and elegant. This is the tree hanging (also known as the snow hanging).

The best time to see fog in a day is in the morning, because fog is formed in the morning, so you should get up early to see fog before the sun comes out. Get up around 5: 00 in the morning, and you will see pine willow frost hanging snow. As the sun rises slowly, you can also take pictures of the red sunrise sprinkled on the white fog pine. The time of disappearance depends on the size of the wind on that day. If the wind is strong that day, it is estimated that it will start to fall at 9 o'clock, and you will be lucky if there is no wind.