What's going on
It's coming down to smoke
In recent days, the sea of shandong and the pyrotechnics have fallen as heavy as snow。
Some netizens say that “smoking” is “smoking” and that, in fact, such snowfalls are called cold-flowing snow. How does the cold snow form? Why do you like weihai
How does the cold snow form
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Cold snow
The so-called cold-flowed snow, also known as cold-flowed snow, is due to the abundance of water vapour at sea, the higher temperature of water on the surface of the sea than on the inland surface during the winter, the relative warmth and humidity of the air above the sea surface, and the rise of warm and wet air above the sea surface to a certain height when the cold air falls south。
Snow
Often in coastal areas
Cold-flowed snow is often found in our yellow sea and the coastal areas of the sea, as well as in the eastern coastal areas of jiangsu, shanghai and liaoning, most typically in the area of the smoke pyrotechnics and the sea of wei, where cold-flowed snow accounts for more than 80 per cent of total snowfall days。
Unlike the general snowfall, cold-flowed snow is fluid, endemic and prone to snow accumulation。
Smokes, weihai
Why is there always cold snow in winter
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Snow bay, china
The two coastal cities in the shandong peninsula, the smoke plateau and the ui hai sea, are known as “china snow peaks” as a result of the unique snowfall in the seaside, due to the winter。
Climate
The snow is mostly cold
Every winter, there is a significant increase in the amount of snow from the pyrotechnics and the sea, as compared to the rest of the mountain, and the two cities are dominated by cold-flowing snow. According to weather statistics from the kitale mountain airport, the average annual number of days of cold-flowed snow in the area is about 39 days。
It's unique
At the eastern end of the mountain peninsula, and on the northern, eastern and southern sides of the yellow sea, it is uniquely located and prone to cold-flowing snow. The high level of snowfall is one of the characteristics of cold-flowing snowfalls, with 80. 3 mm of precipitation in the smoked tsetse area from late 2005 to early 2006。
High ocean heat capacity
The high heat capacity of the ocean, the much more moderate changes in the temperature of the sea during the winter, and the much more moderate changes on land. The cold air in the south passes through the sea of the sea of the sea of the sea of the sea, and the warmer and more humid atmosphere of the lower layer of the air provides conditions for air-to-flow movements to form a somewhat transient layer of clouds on the seashore and generate snow。
Topography lifts and coast frictions
The rise in the topography of the northern coast of the peninsula and the friction on the coast will quickly lift the warm and wet gas stream above the condensed height and will also increase the impact of cold-flow snow。
Warm and warm
Some pictures are generated by ai
Edit, design / wang lin
