1, the mountains are shrouded in fog, like silk covered with fine gauze, looming.
2. The fog slowly flows down from the mountain, like strips of white gauze fluttering in the air.
The fog on the mountain seems to be wrapped in a layer of gauze, and it is as hazy as a layer of gauze.
4, Dieyun around the mountain. The trees and flowers on the mountain were shrouded in a veil-like mist and blurred in the smoke.
5. The mountains are foggy and the trees are looming. The mountain peak in the distance sometimes looks like a dragon, lying between heaven and earth; Sometimes a slim girl, wearing a thin veil, faces the morning sun.
A poem describing the misty mountains;
1, the cloud is not * * * this mountain is neat, and the mountain is hazy and gray. At dawn, the crescent moon flies to the tall trees, and the Milky Way in autumn night is far to the west of several peaks.
Its huge height is close to the city of heaven, connecting a thousand mountains and a corner of the sea. The white clouds merged behind, and the blue mist melted into the mountains and disappeared.
3. The misty Kosashige, the mountains and rivers are deep here. In autumn, the sound of the beach is more urgent and the canyon is overcast.
4. How deep the courtyard is, the cloud window and fog pavilion are in late spring. For whom you are haggard and lose your face, and you have a good night dream, you should send Nanzhi.
5. The sky meets the clouds, and the Milky Way wants to turn to Qian Fan dance. As if the dream soul belonged to the emperor.
Fog:
Fog is a common weather phenomenon, which refers to water vapor condensate composed of water droplets or ice crystals suspended in the atmosphere near the earth's surface. When the temperature reaches the dew point temperature (or near the dew point temperature), the water vapor in the air condenses to form fog. The difference between fog and clouds is that clouds are produced in the upper atmosphere, while fog is close to the surface.
There are several different types of fog according to the cause of condensation. When the temperature is above freezing point, water vapor condenses into water droplets. When the temperature is below freezing point, water vapor condenses directly into solid ice crystals, such as ice fog.
Because the dew point is only affected by air temperature and humidity, there are two main reasons for the formation of fog: first, the water vapor in the air increases greatly, which makes the dew point rise to the air temperature, thus forming fog, such as steam fog and frontal fog; Second, when the temperature drops below the dew point, fog is generated, such as advection fog and radiation fog.
Fog mostly appears between February and April in spring. Forming conditions: cooling, humidifying and increasing water vapor content. There are radiation fog, advection fog, mixed fog and evaporation fog.