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Which city does Wudi County belong to?
Wudi County belongs to Binzhou City.

Wudi County, which belongs to Binzhou City, Shandong Province, is located in the north of Shandong Province, bordering Bohai Bay in the northeast, Zhanhua District in the southeast, Yangxin County in the south, Qingyun County in Dezhou City in the west, Haixing County and Huanghua City in Cangzhou City, Hebei Province in the north. It is located between 37 4-38 N/KOOC-0/6 E/KOOC-0/7 3/KOOC-0/-KOOC-0//KOOC-0/8 04, with a total area of 2,089.77 square kilometers./KOOC-. Jurisdiction over 2 streets, 10 town.

Wudi County has two sub-district offices, six towns, 1 state-owned farms and * * * 107 administrative villages. Sub-district offices: Chengguan and Weiwan; Towns: Lucun Town, Kangzhuang Town, Linzi Town, xin zhuang zhen, Jinjizhuang Town and Xiyan Town. Wudi County is a county-level administrative unit under the jurisdiction of Binzhou City, Shandong Province. Binzhou City is located in the north-central part of Shandong Province, with 9 municipal districts and 2 counties under its jurisdiction. Wudi County is one of the jurisdictions of Binzhou City.

Introduction to the geography of Wudi County:

1, landform

Wudi County is a floodplain in the northwest of Shandong Province in the North China Plain. The terrain is high in the southwest and low in the northeast. The highest point is in the west of Haifeng Street, with an altitude of 8 meters (the altitude of the Yellow Sea, the same below), and it inclines to the northeast with a slope of110000. Coastal Dakou River, elevation1.9m; The elevation of Sanlitai and Wulitai along the coast is only about 1 meter. From southwest to northeast, the territory is yellow flood plain, coastal plain and Bohai Bay coast in turn. Jieshi Mountain is the only hill north of the Yellow River in Binzhou City, located at the junction of the Yellow River Plain and the coastal plain in northern Binzhou.

2. Climate characteristics

Wudi County belongs to the continental climate of the East Asian monsoon region in the north temperate zone, with four distinct seasons and obvious dryness and wetness. It is windy and dry in spring, wet and rainy in summer, crisp in autumn and long, dry and cold in winter. In spring (March-May), warm air began to increase actively, cold and warm air came one after another, and the high-pressure system moved frequently, resulting in changeable climate and less rainfall, accounting for only 13.7% of the annual precipitation. The average temperature in March is 6.9℃, which can rise to 20. 1℃ in May. Because of less wind and rain and rapid evaporation, spring drought often occurs.

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