Complete collection of detailed information in southern China.

The southern region refers to the southern part of the monsoon region in eastern China, which is one of the four geographical divisions in China today. It is mainly the area south of the Qinling-Huaihe line, with the Qinghai-Tibet Plateau in the west, the Yellow Sea, the East China Sea and the South China Sea in the east and south, respectively. The length of the mainland coastline accounts for more than two thirds of the country.

Administrative divisions include most of Jiangsu, most of Anhui, Zhejiang, Shanghai, Hubei, Hunan, Jiangxi, Fujian, most of Yunnan, Guizhou, eastern Sichuan, Chongqing, southwestern Shaanxi, Guangxi, Guangdong, Hong Kong, Macau, Hainan, Taiwan Province, southeastern Gansu, Xinyang, Henan and Nanyang.

The area accounts for about 25% of the land area, the population accounts for about 52% of the country, and the Han nationality accounts for the majority. There are more than 30 ethnic minorities in the whole region, with a population of more than 50 million, mainly distributed in Yunnan, Guizhou, Sichuan, Chongqing, Hunan, Guangxi, Qiong and other places, with a large number of Zhuang, Miao, Yi, Tujia, Buyi, Dong, Bai, Hani, Dai and Li nationalities.

Basic introduction Chinese name: mbth, Southern China: South China alias: South China administrative region category: geographical division area: South China's jurisdiction areas: Jiangsu, Anhui, Shanghai, Zhejiang, Fujian, Guangdong, Qiong, Hubei, Hunan, Jiangxi, Sichuan, Chongqing, Yunnan, Guangxi, Hong Kong, etc. Telephone area codes: 020, 02 1. 028,0571,0755 and other postal codes: 200000, 2 10000, 3 10000, 5 10000, 6 10000 and other geographical locations: Qinling Mountains. Population: about 720 million dialects: Southwest Mandarin, Jianghuai Mandarin, Wu dialect, Xiang dialect, Cantonese, Min dialect and other climatic conditions: subtropical monsoon climate, tropical monsoon climate, equatorial monsoon climate. Famous scenic spots: Bund, Sun Yat-sen Mausoleum, Huangshan Mountain, West Lake, Baiyun Mountain, Gulangyu Island, Dujiangyan, Sun Moon Lake and other airports: Pudong Airport, Tianhe Airport, Baiyun Airport, Shuangliu Airport, Lukou Airport, Xiaoshan Airport and other railway stations: Shanghai Hongqiao Railway Station, Guangzhou South Railway Station, Nanjing South Railway Station, Wuhan Railway Station, Chengdu East Railway Station, hangzhou east railway station and other major cities: Shanghai, Jiangsu, Anhui, Zhejiang. Universities in Macau: Wuda University, Fudan University, Nanda University, Zhejiang University and Zhong Da University. Highest building: Shanghai Center (632m) Country: China people * * * Analyze the concept of country, natural division, administrative division, topography, landforms, climate characteristics, basic characteristics, summer monsoon, quasi-static front of Kunming, specific classification, hydrological conditions, rivers and lakes. Conceptual differentiation of major industrial areas and natural divisions The concept of "southern region" refers to the southern part of the eastern monsoon region of China, mainly referring to the Kyushu region south of the Qinling-Huaihe line, bordering the East China Sea in the east and the South China Sea in the south. Including most of Jiangsu, most of Anhui, Zhejiang, Shanghai, Hubei, Hunan, Jiangxi, Fujian, most of Yunnan, Guizhou, eastern Sichuan, Chongqing, southwestern Shaanxi, Guangxi, Guangdong, Hong Kong, Macau, Hainan, Taiwan Province, southernmost Gansu, Nanyang, Henan and Xinyang. The area accounts for about 25% of the country, the population accounts for about 55% of the country, and the Han nationality accounts for the majority. Most of the ethnic minorities with a large population live in southwest and south-central regions. There are more than 30 ethnic minorities in this area, with a population of more than 50 million, mainly distributed in Guangxi, Yunnan, Guizhou, Sichuan, Hunan and Qionglai, among which Zhuang, Miao, Yi, Tujia, Buyi, Dong, Bai, Hani, Dai and Li have a large number. It is generally believed that the Qinling-Huaihe line is the northern boundary of the "southern region" in China's natural division. 1908, Zhang, the first president of the former geographical society of China, first proposed "Huaishui in Beiling" as the "north-south dividing line" in the book "Newly Written Geographical Documents". At that time, the northern ridge corresponding to Nanling was Qinling Mountain. Most contemporary scholars believe that Qinling-Huaihe River is not a simple geographical boundary between north and south of China, but a geographical and climatic boundary between north and south of China. Because the concept of natural zoning is widely used in basic education in China, this entry is mainly based on the concept of natural zoning. The concept of administrative division in southern China based on natural division includes southeast, south-central and southwest China. Including Jiangsu, Anhui, Shanghai, Zhejiang, Fujian, Jiangxi, Hubei, Hunan, Sichuan, Chongqing, Yunnan, Guizhou, Tibet, Guangxi, Guangdong, Hainan, Taiwan Province, Hong Kong and Macau. Different from natural division in different degrees. South of Qinling Mountains in southern Shaanxi, Xinyang and Nanyang in Henan, and the southern end of Gansu belong to the southern region of natural division. Northern Jiangsu and Anhui, Tibet, western Sichuan and northern Yunnan do not belong to the southern regions of natural division. The terrain in this area is high in the west and low in the east. The terrain is plain, basin and plateau, located at the second and third steps, and the hills are staggered. There are many rivers and lakes in the plain area, and the water network is vertical and horizontal, which has typical characteristics of southern water towns. Most mountainous and hilly areas have lush vegetation and beautiful scenery. There is a great difference between the east and the west in the southern part of the terrain, mainly located in the second and third steps, with vast plains and hills in the east. The plain in the middle and lower reaches of the Yangtze River is the lowest-lying area in China, with criss-crossing rivers and tributaries and dotted with lakes. The hills in the south of the Yangtze River are the largest in China, and most of them are distributed alternately with low mountains and valley basins in the northeast-southwest direction. Magmatic rocks are widely distributed in Nanling area; The western part is dominated by plateaus and basins, and Sichuan Basin (Chengdu Plain in the northwest, also known as "Land of Abundance") is one of the four great basin in China. Yunnan-Guizhou Plateau has a rugged surface, which is the most typical karst landform distribution area in the world, and the mountain "bazi" is the main agricultural area in this area. Hengduan Mountains and Qinling Mountains are important geographical boundaries of China. The main topographical areas are: the middle and lower reaches of the Yangtze River plain (Jianghan, Dongting Lake, Poyang Lake and Yangtze River Delta), the Pearl River Delta plain, the hills in the south of the Yangtze River, the Sichuan Basin, the Yunnan-Guizhou Plateau, the Hengduan Mountains, the Nanling Mountains, the Wuyishan Mountains, the Qinba Mountains, the central mountainous areas of Taiwan Province Province, the hills of Guangdong and Guangxi, and the Dabie Mountains. Basic climate characteristics The southern region is dominated by tropical and subtropical monsoon climate, with high temperature and rainy summer and mild and little rain in winter. Among them, the tropical monsoon climate is hot all year round, divided into dry season and rainy season. The precipitation is above 800 mm, and there is more precipitation on the windward slope of the mountain. Huoshaoliao in Taiwan Province Province is the "rain pole" of China, with an average annual precipitation of 6558 mm.. The eastern coastal areas are greatly affected by typhoons in summer and autumn. The temperature is above 0 degrees in winter. Leizhou Peninsula, Yunnan, southern Taiwan Province Province and Hainan are above 15 degrees. Yunnan, Guangdong, Hainan and Taiwan Province provinces are less affected by the cold wave. The southern part of the summer monsoon is greatly influenced by the summer monsoon, and the rainy season is longer. Every May, the summer monsoon enters from the coast of South China, and the rainy season begins. From June to July, the summer monsoon forces strengthened and moved northward, forming a quasi-static front between the Yangtze River and the Huaihe River, and the rainy weather continued, mainly affecting the middle and lower reaches of the Yangtze River and the Huaihe River basin. Summer drought is easy to form in July and August. In September, the rainfall front moved south to this area, and after 10, the cold air force was further strengthened, the summer monsoon moved out of this area, and the rainy season ended. In addition, the southwest region is often affected by the southwest monsoon. The cold air in the north of Kunming quasi-static front and the southwest airflow are blocked by topography, and continuous rainy weather often occurs. It appears in the winter half year, between Kunming and Guiyang. The specific classification is (1) equatorial monsoon climate. Located in the South China Sea Island area south of north latitude 10 degrees. The annual average temperature is above 26℃, the annual accumulated temperature reaches 9000℃, the temperature changes little, and the rainfall distribution in the four seasons is relatively uniform. (2) Tropical monsoon climate. Including southern Taiwan Province Province, Leizhou Peninsula and Hainan Island. The annual accumulated temperature is ≥ 8,000℃, the average temperature in Leng Yue is not lower than 16℃, the annual extreme minimum temperature is not lower than 5℃ on average for many years, and the extreme minimum temperature is generally not lower than 5℃, and there is no frost all year round. (3) Subtropical monsoon climate. It is mainly distributed in the south of Huaihe River in Qinling Mountains in eastern China, north of tropical monsoon climate type and east of Qinghai-Tibet Plateau. The average temperature in Leng Yue in winter is around 0℃. Summer is hot, the average temperature in the hottest month is above 22℃, and the temperature changes obviously in seasons with four distinct seasons. The annual precipitation is generally 1, 000 ~ 1, 500mm, which is more in summer, but there is no obvious dry season. Compared with the temperate monsoon climate, the seasonal changes are basically similar, except that the winter temperature is relatively high and the annual precipitation increases. The annual accumulated temperature is 4500℃~ 8000℃, and the average temperature in Leng Yue is -8℃~ 0℃, which is a transitional zone between tropical and temperate zones, and the summer temperature is quite high (average temperature >; =25℃ for at least 6 days, i.e. 30 days). Hydrological conditions Under the natural division of rivers, the main rivers are Yangtze River, Xijiang River, Huaihe River, Qiantang River and Minjiang River. Its main characteristics are large water quantity, long flood season, small sediment concentration, no ice age, rich water resources and high shipping value. Among them, the Yangtze River is called the "golden waterway" because of its shipping value. There are many lakes in Hunan, and the middle and lower reaches of the Yangtze River are the most concentrated. There are mainly Poyang Lake, Dongting Lake and Taihu Lake. Poyang Lake: Located in the north of Jiangxi Province and the south bank of the Yangtze River, it is the largest freshwater lake in China and the second largest lake in China. Dongting Lake: Located in the north of Hunan Province, south of Jingjiang reach of the Yangtze River, it is the third largest lake and the second largest freshwater lake in China (the original largest freshwater lake has retreated to the second freshwater lake due to continuous shrinkage). Taihu Lake: Located at the junction of Jiangsu Province and Zhejiang Province. The third largest freshwater lake in China. Main agricultural commodity grain bases: Yangtze River Delta, Jianghuai Plain, Jianghan Plain, Chengdu Plain, Poyang Lake Plain, Dongting Lake Plain and southern Pearl River Delta: southern sugarcane, rape, cotton, tea and other crops; Sugar crops in the south: oil crops in the south of sugarcane: camellia oleifera, tung oil and rape; Southern land use: paddy fields, transportation, inland river transportation: Yangtze River, Beijing-Hangzhou Canal, etc. Railway is the main traffic map in the south: North and South: Beijing-Shanghai (Beijing to Shanghai), Beijing-Guangzhou (Beijing to Guangzhou), Beijing-Kowloon (Beijing to Hong Kong), Liu Jiao (Jiaozuo to Liuzhou), Cheng Kun (Chengdu to Kunming), Baocheng (Baoji to Chengdu) and other international airports are Shanghai. China traditional opera art: Kunqu opera, Cantonese opera, Huangmei opera, Yue opera, Baiju opera, Yangju opera, etc. Crafts: Yunjin, Shu embroidery, Su embroidery, Yang embroidery, etc. Non-ferrous metals with resource advantages-tungsten in Dayu, Jiangxi, copper in Dexing, antimony in tin mine in Hunan, lead and zinc in Shuikoushan, aluminum in Pingguo, Guangxi, mercury in Tongren, Guizhou, copper in Dongchuan, Yunnan, and Shangtianti nonmetallic mine in Xinyang, Wuxi-Puguang gas field in Dazhou, Sichuan, are the largest gas fields in Asia. Iron and steel-Panzhihua in Sichuan, Daye in Hubei, Maanshan in Anhui, Shilu in Hainan and Wuhan Coal Industry-are less. Anhui Huainan, Guizhou Liupanshui and southern Sichuan Luzhou are rich in hydropower. Three Gorges, Gezhouba, Geheyan, Danjiangkou, Ertan, Yantan, Wuqiangxi, Wujiangdu and Shuikou nuclear energy-forest resources of Zhejiang Qinshan Nuclear Power Station, Guangdong Daya Bay and Ling 'ao Nuclear Power Station-southwest forest region, main industrial zone of southeast plantation 1, industrial zone along the Yangtze River and Shanghai-Nanjing-Hangzhou Industrial Zone are the largest comprehensive industrial bases in China. 2. The Pearl River Delta is a light industrial area in China.