Is Zhuozhou a flood discharge area?

Zhuozhou is not a flood discharge area.

Zhuozhou is located in the south of Beijing and belongs to the first line of Taihang East Road in Baoding, Zhuozhou. Although Zhuozhou is a flooded place, it is not within the scope of flood discharge. Flood discharge is to protect downstream areas. Zhuozhou is not a downstream area, but it is located in the flood discharge range of Taihang East Road. For this flood, just look at the rainfall map and you will know that the whole river along Taihang East Road is discharging flood. If the flood is not drained, Zhuozhou and the area south of Zhuozhou will suffer more disasters.

The flood discharge area of this flood is mainly located in the flood storage area of Tianjin, because the rivers in the rainstorm area basically enter the sea from Tianjin. Therefore, it is unfounded to say that Zhuozhou flood discharge will flood the rainstorm area.

Brief introduction of geographical environment in Zhuozhou;

1, landform

The terrain of Zhuozhou City is generally characterized by high in the west and low in the east, and the terrain is relatively flat. The whole territory is located in the front inclined area of Taihang Mountain, which inclines from northwest to southeast. The highest altitude is 69.4m, the lowest altitude is 19.8m, and the ground slope is about 1/660. The landform is influenced by the alluvial of Juma River, and there are two terraces in the north and south, with the height difference ranging from 2 to 4 meters.

2. Climate

Zhuozhou belongs to the warm temperate semi-humid monsoon region, with obvious continental monsoon climate characteristics, large temperature difference and distinct four seasons. In Zhuozhou, the sunshine hours in spring are gradually prolonged, the ground temperature rises rapidly, and the inland low pressure activities are frequent. However, the dry and cold air in the north is still going south, which continues to have an impact on Zhuozhou, so the wind is dry. In summer, affected by the subtropical high in the North Pacific, the summer monsoon blowing from the ocean to the mainland is prevalent, humid and rainy.

In autumn, the Pacific subtropical high center moves eastward, the westerly wind prevails, the summer heat subsides, the temperature gradually drops, and the gas layer is relatively stable. Therefore, the weather of "clear clouds and clear wind, clear sky" often appears. In winter, influenced by Mongolia's strong high pressure, the northwest wind blowing from the inland to the ocean prevails, with little rain and snow, cold and dry.

3. Hydrology

There are many rivers in Zhuozhou, including Yongding River, Baigou River, Xiaoqing River, Liuli River, BeiJuma River and Huliang River, which belong to Haihe River Basin and Daqinghe River System.

The above content reference: Baidu Encyclopedia-Zhuozhou City