After the heavy rain, there was a sea of clouds in the mountains. How is it formed and what are the rules?

The sea of clouds will only appear after rain and snow. So the season with the highest sea of clouds is winter and spring, that is, June 12, 1, February, March, April, May and June, and the season with the highest rainfall is also the season with the highest sea of clouds. The relative sea of clouds will be relatively low in the middle and late years of each year, and the month with the highest sea of clouds in June 12 will be particularly high compared with April and June. In other words, experts say the rainy season and now are the most likely. In winter and spring, the air temperature in the middle and lower layers is low, the condensation height of stratocumulus is low (about 800 ~ 1200m), and cold air activities are frequent. The weather activity is obvious during the process. After rain and snow, there will often be a large area of good sea of clouds, especially the spectacular sunrise of the sea of clouds. In the rainy season after summer, with the temperature rising, the condensation height of clouds rises to about1500m, and the height of clouds exceeds or approaches most peaks. At this time, the clouds are shrouded and it is difficult to see the sea of clouds. July-August is the midsummer of Huangshan Mountain. During this period, it is often controlled by the Pacific subtropical high, the temperature rises, and the condensation height of low clouds also rises to the highest level in the whole year. The shady side of the mountain is humid and prone to convection. From morning to afternoon, light cumulus clouds and thick cumulus clouds often form around the mountain, but because the clouds are higher than the summit, the sea of clouds is rare. In the evening or morning, you can occasionally see a sea of clouds formed by cumulus and stratocumulus, but they are easily destroyed due to the influence of circulation, and the sea of clouds lasts for a short time. After autumn, affected by the cold air in the north, the temperature drops and the condensation height of low clouds also drops. After the cold air, there will often be a large sea of clouds with high stratocumulus.