Traditional Culture Encyclopedia - Weather forecast - On-site exposure of Kaijiang River in Jiamusi section of Songhua River. Why is this happening?

On-site exposure of Kaijiang River in Jiamusi section of Songhua River. Why is this happening?

The Jiamusi section of Songhua River opens because with the coming of spring, the frozen river surface changes due to the rising temperature, and sometimes it gradually melts due to the slow rising temperature, and the ice cubes flow down the river, forming a spectacular ice running landscape. Wen Kaijiang? Present in the form of. But sometimes, due to the sudden rise of temperature, the frozen river surface bursts overnight, and the ice deposits overlap, and a large number of ice cubes pile up ashore. With what? Wu Kaijiang? Present in the form of.

The spectacular scenery of Kevin River and Wukai River.

Wenkaijiang and Wukaijiangdu are Kaijiang dialects in kanto region, and the reasons for their formation depend on the climate in that spring, the rapidity of the river and other factors. Many people will come to see it during the river opening. From a distance, a large number of dense ice cubes are floating on the wide river, and rows of ice cubes flow down the river. Close up, with the movement of the ice, people not only feel a little dizzy, but also the sound of the ice becomes crisp and pleasant with the impact, like a crystal falling to the ground. Another example is the arrival of thousands of troops from Ma Benteng, with great momentum and full of energy. As the process of opening the river draws to a close, the river is no longer frozen and full of vitality, and the river shines in the spring breeze. Freed from the cold, a warm and brand-new new year has come again, which only Kanto people can realize, and it is a special feeling for spring.

This year, the Songhua River opened in the form of Wu Kaijiang.

Judging from the shape of Wukai River, it shows that the temperature of Songhua River has risen sharply this year. In the video sent by netizens, we can see that large and thick ice blocks have been washed up on the river bank, and ice walls as high as two or three meters have been piled up. Although the flood is like a beast, this ice wall is like a monster. Because the ice was too slippery, some smaller ones were thrown to the shore a few meters away. Such a scene is also very dangerous, reminding tourists to stay away from the river to watch in case of being injured by ice. Whenever a large amount of ice comes ashore, many people take pictures, leaving wonderful moments, bringing fresh visual impact and experience, which is very exciting. Netizens who have never been to the northeast have also said that this scene is amazing and it is the first time to see it.

When the water level in Kaijiang River rises, the relevant departments issue a yellow warning of ice flood, and the public pays attention to strengthening prevention.

With the arrival of Kaijiang River, the water level of Songhua River began to rise. The water level of Kaijiang River is 77.23 meters, and it reaches 79.3 1 meter in the evening, which exceeds the warning water level and reaches the release standard of yellow flood warning. Relevant departments have also issued a warning notice of ice flood. Due to the fact that the upper reaches of Xinjiang haven't completely melted, the water level of Jiamusi section of Songhua River has been consistent, rising to 79.77438. 10000000075. Although the water level dropped later, it was still 79.56 meters higher than the warning water level. Officials from relevant departments also said that the water level in the upper reaches will continue to rise in turn because the dam is still blocked by silt. I can only hope that the temperature will rise faster, so that the ice in the downstream will melt quickly and the water will be washed away by the downstream, so that the water level will drop, the water level will rise, and the ice will be discharged quickly, which will also cause certain impact and damage to the ships and docks along the coast. relevant department

?

?

?