If the Mongolian cyclone affects the weather in China

generally, its moving path is slightly south to the east, passing through the west of Xilin Gol League, and moving along the northeast plain and the Songhua River. The other two are moved eastward via Hulunbeier League and southeast via North China and Bohai Sea, and around Changbai Mountain via North Korea. It shows a variety of weather, among which strong winds are the main ones.

Strong winds and less precipitation

Strong winds can be found in any part of the Mongolian cyclone. The precipitation is generally small, even < P > not at all, because the warm air in the cyclone mostly comes from the northeast of the Qinghai-Tibet Plateau and the Hexi Corridor, and the water vapor is insufficient. Usually, except for some precipitation in the north of the center, most other areas only have high clouds. It is worth noting that the activity of Mongolian cyclone is always accompanied by the invasion of cold air, so the weather phenomena such as strong wind, sandstorm and frost follow.