Traditional Culture Encyclopedia - Weather forecast - Administrative divisions of Nanzheng county
Administrative divisions of Nanzheng county
20011/With the approval of the Shaanxi provincial government, some towns and villages were merged, and counties administered 18 and 12 towns. There are 50 1 administrative villages below the township level, and there are 3805 villagers' groups below the village level.
In April 2002, 14 community neighborhood committees were established. From June, 5438 to February, 2002, according to the Notice of the Municipal Party Committee and the Municipal Government on Printing and Distributing the Implementation Plan for Straightening the Management System of Hanzhong Economic Development Zone, Hanzhong Civil Affairs Bureau divided six villagers' committees, including Dingshuying Village, Dongjiaying Village, Kangjiaying Village, Sujiashan Village, Huilongsi Village and Zhangjia Village, belonging to Dahekan Town of Nanzheng County, and established the Southern District Office of Hanzhong Economic Development Zone, which was placed under the jurisdiction of Hanzhong Economic Development Zone. There are 495 administrative villages and 13 neighborhood committees below towns and villages; There are 3770 villagers' groups below the village.
On June 24th, 20 1 1, according to the official reply of Hanzhong Civil Affairs Bureau on the administrative division adjustment plan of withdrawing towns and merging towns, the county was merged from 30 townships into 22 towns, and from 3762 villagers' groups in 495 administrative villages into 3054 villagers' groups in 393 administrative villages. So far, there are 22 towns, 393 administrative villages, 14 community neighborhood committees and 3054 villagers' groups in the county. Nanzheng county belongs to the north subtropical humid climate zone. Due to the influence of geographical factors and monsoon circulation, the climate has the following characteristics:
① Located at the boundary between land and sea climate, it includes two climatic zones, namely the north subtropical zone and the warm temperate zone, especially the north subtropical zone.
② It has obvious monsoon climate characteristics. Winter is controlled by Mongolian high pressure, often dry and cold air flows in, the weather is cloudy, dry and rainy, and there are more northeast winds, but the wind is weak; There is a cold wave, but the temperature is not too low. Spring is the season when dry and cold air flows in the north alternate with hot and humid air flows in the south. At first it was warm and cold, and the weather was changeable. During the Qingming Festival, there are many rains and yellow sand bursts. In summer, southeast monsoon activities are frequent, hot and humid airflow enters, rain and heat are in the same season, and thunderstorms are often accompanied by strong winds; Drought happens from time to time. In autumn, the cold air mass in the north meets the warm air mass in the south, and it often rains continuously in the territory, sometimes the land is not dry all month; But sometimes the weather is dry (commonly known as "autumn tiger"). This feature is one of the factors that lead to less sunshine hours in autumn.
(3) Affected by topography, the vertical difference between temperature and precipitation is significant: the temperature on the northern slope of Micang Mountain decreases from north to south; From north to south, the precipitation is increasing.
(4) Severe weather such as rainstorm, low temperature, continuous rain and drought frequently occurs.
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