The weather in Qiyao Mountain

Wanzhou District is located in the eastern edge of Sichuan Basin and the northeast edge of Chongqing, with east longitude10755' 22' ~10853' 25'' and north latitude 30 24' 25' ~ 314' 58''. Yunyang in the east, Shizhu and Lichuan in Hubei in the south, Zhongxian and Liangping in the west and Kaijiang and Kaixian in the north. It is 97.25 kilometers wide from east to west, 67.25 kilometers long from north to south, and covers an area of 3,457 square kilometers (the cultivated land area is 6,543,800 mu, including 584,900 mu; The sloping land above 25 degrees is 50 1.400 mu, including 324,900 mu of dry land), with an urban area of 32.5 square kilometers and a linear distance of 228 kilometers from Chongqing. The hills in this area are undulating. The highest point is Shaping Peak in Baozi Township, with an altitude of1.762m; The lowest point is Huangbai Township, with an altitude of1.006m; The northwest is Xiaoyakou, Fengshanliao, Goldman Sachs Township, with an altitude of 1, 373.3 meters; The relative height difference in China is1.84.5m and1.266m respectively. The rivers in the territory are vertical and horizontal, and the rivers and streams are deeply cut, with large drop and wide height, which are tributaries, all of which belong to the Yangtze River system. The Yangtze River enters from Shicaoxi (elevation 1 18m) in Changping Township at the junction of Shizhu and Zhongxian County in the southwest, crosses the hinterland to the northeast, flows into Yunyang County through Baishuitan (elevation 106m) in Huangbai Township, with a flow of 80.4km .. Rivers with an area of over 65,438+000km2 in China Basin are north of the Yangtze River. There are 93 gullies in Nixi River, Wuqiao River and Xintian River south of the Yangtze River, with a total water area of 65,438+063,000 mu (65,438+008.66 square meters). The geological ages of exposed strata in China are mostly seen in Mesozoic Triassic and Jurassic, which were formed 23 ~137 million years ago, among which Jurassic is the most widely distributed, followed by Triassic and Paleozoic Permian strata 285 ~ 230 million years ago and Cenozoic Quaternary strata 2.5 million years ago in some places, and China's geological structure line. Sichuan rhombic tectonic basin belongs to the western edge of Wulingshan fold belt and Dabashan arc fold belt, the third largest uplift belt in Xinhua Xia, extending from northeast to northeast and disappearing in the northwest of Qiyaoshan anticline structure, forming Wanxian arc structural line protruding to the northwest. Wanzhou district belongs to subtropical monsoon humid area, with four distinct seasons and warm and foggy winter. Summer is hot and dry; In early spring, the temperature rises rapidly and is unstable. In autumn, it is long and rainy, with abundant sunshine and rainfall, mild weather, long frost-free period and scarce frost and snow. The annual average temperature in China 17.7℃, the highest annual average temperature 19.0℃( 1982) and the lowest annual average temperature 176℃( 1974). The extreme maximum temperature for many years is 41℃ (1August 26th, 972), and the extreme minimum temperature is-3.7℃ (65438+1October 27th,1975+February 15). The average annual sunshine hours for many years are 1, 484.4 hours, the maximum sunshine hours are 1, 7 1.3 hours, and the minimum sunshine hours are 924 hours. According to the statistics of Datankou Station in China, the average annual precipitation is1.243mm, the maximum annual precipitation is1.549.6mm (65438+ the minimum annual precipitation is 981.9mm (1976), the average annual water surface evaporation is 620mm, and the total annual evaporation reaches.