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Comparison between Hubei weather and Shanghai weather

Beijing has a temperate monsoon climate with the following characteristics: cold and dry in winter; Summer is warm and rainy.

Tianjin is located on the east coast of mid-latitude Eurasia and is controlled by monsoon circulation. This is an area where East Asian monsoon prevails and has a continental climate. The main climatic characteristics are: four distinct seasons, windy spring, drought and little rain; Summer is hot and the rain is concentrated; Autumn is cool and the temperature is moderate; Winter is cold, dry and snowy.

The northern province is located on the east coast of Eurasia in the middle latitude and the east coast of China, and belongs to the temperate humid and semi-arid continental monsoon climate. In most parts of this province, the four seasons are distinct, the difference between cold and summer is wide, the rainfall is concentrated, the wet and dry periods are obvious, the winter is cold and dry, and the rain and snow are scarce. Spring is changeable, dry and windy; Summer is hot and humid, with concentrated rainfall; Autumn is sunny, cool and rainy.

The climate characteristics of Shanxi: long face is cold and dry in winter; Summer is short, hot and rainy; In spring, the daily temperature difference is large and there are many sandstorms; Autumn is short and the weather is mild. Shanxi province belongs to the temperate monsoon climate zone, that is, the temperate continental climate.

Inner Mongolia belongs to a typical mid-temperate monsoon climate, which is characterized by less and uneven precipitation and drastic changes in temperature and warmth.

Liaoning is located on the east coast of Eurasia and in the mid-latitude zone, so the climate type still belongs to temperate continental monsoon climate. However, due to the complex terrain, including mountains, plains, hills and coastal areas, the climate in different parts of the province is not the same. However, the general climatic characteristics are: long cold period, strong wind in the plain, wet in the east and dry in the west, concentrated rainfall, abundant sunshine and distinct four seasons.

Jilin Province is located in the mid-latitude zone of the northern hemisphere, in the east of Eurasia, which is equivalent to the northernmost temperate zone in China and close to the sub-frigid zone. The east is close to the Yellow Sea and the Sea of Japan, and the climate is humid and rainy. The west is far from the ocean and close to the dry Mongolian plateau, with a dry climate. The province has formed a remarkable temperate continental monsoon climate, with four distinct seasons and the same season of rain and heat. There are obvious seasons, which are dry and windy in spring, hot and rainy in summer, crisp in autumn and long and cold in winter.

Heilongjiang Province is located on the eastern edge of Eurasia in mid-latitude, on the west coast of the Pacific Ocean, adjacent to cold Siberia in the north and across the temperate zone in the north and south. Therefore, the climate of Heilongjiang province has obvious monsoon climate characteristics, but the western part is weakly affected by the summer monsoon, showing some continental climate characteristics.

Shanghai has a subtropical maritime monsoon climate. The main climatic characteristics are: warm in spring, hot in summer, cool in autumn and cold in winter, moderate annual rainfall and relatively even seasonal distribution. Generally speaking, the climate is mild and humid, with four distinct seasons.

Jiangsu Province is located in the eastern coast of Chinese mainland, in the transitional climate zone between subtropical zone and south temperate zone, with obvious monsoon characteristics, distinct four seasons, synchronous rain and heat, concentrated rainfall, abundant sunshine, superior natural conditions and abundant climate resources. Influenced by the westerlies, subtropics and intertropical convergence zone weather systems, the climate is complex and disastrous weather is frequent.

The climate in Zhejiang is characterized by obvious monsoon, distinct seasons, moderate annual temperature, abundant sunshine, abundant rainfall, moist air, synchronous seasonal changes of rain and heat, diverse allocation of climate resources and numerous meteorological disasters.

Anhui is located in the mid-latitude zone. Under the comprehensive influence of solar radiation, atmospheric circulation and geographical environment, Anhui has a transitional climate from warm temperate zone to subtropical zone. In the climate division of China, the north of Huaihe River belongs to temperate semi-humid monsoon climate, and the south of Huaihe River belongs to subtropical humid monsoon climate. The main climatic characteristics are: obvious monsoon, distinct seasons, mild climate, moderate rainfall, changeable temperature in spring, fresh air in autumn, obvious plum rain and concentrated rain in summer.

Fujian is located in the southeast of the motherland, on the coast of the East China Sea. It belongs to subtropical humid monsoon climate. There are mountains in the northwest to block the cold wind, and the southeast is regulated by the sea breeze. A warm and humid climate is a remarkable feature of the climate. Taking Fuzhou-Fuqing-Yongchun-Zhangping-Shanghang as the boundary, it can be divided into middle subtropical zone and south subtropical zone. Its main features are as follows: First, the monsoon climate is remarkable. The cold and warm climate, the beginning and end of the four seasons, all shift with the activity of monsoon circulation. Second, winter is short and summer is long, with abundant heat resources. Third, the winter is warm, and the temperature difference between north and south is large; It is cool in summer, and the temperature difference between north and south is small. Fourth, the rainy season and dry season are distinct, and water resources are abundant. Fifth, complex terrain leads to diverse climate.

Jiangxi is located near the Tropic of Cancer, which warms up earlier in spring, but the weather is changeable, from warm to cold, with more rainfall until early summer. It was sunny, hot and dry before midsummer to Mid-Autumn Festival. It is very cold in winter, but the frost period is short.

Shandong's climate belongs to warm temperate monsoon climate type. Precipitation is concentrated, rain and heat are in the same season, spring and autumn are short, winter and summer are long.

He 'nan Province is located in the eastern monsoon region of China, spanning two natural units: warm temperate zone and north subtropical zone, with latitude 3 1' ~ 1L6 39' and longitude LL0 2 1'. The climate is mild and has obvious transitional characteristics. There is a significant difference between the north and the south, and there are also significant differences between the mountains and plains. There are four distinct seasons throughout the year. The general climate features are: cold in winter, little rain and snow, drought and little sandstorm in spring, hot and rainy in summer, abundant sunshine in autumn and long sunshine time.

The geographical location of Hubei Province is between 29 05 ′ ~ 33 20 ′ north latitude and108 21′ ~16 07 ′ east longitude, which mainly belongs to the north subtropical monsoon climate and has the characteristics of transition from subtropical to warm temperate zone. Sufficient sunshine, sufficient heat, long frost-free period, abundant precipitation and the same season of rain and heat are beneficial to agricultural production. There is a folk saying that "the lake is wide and ripe, and the world is full."

Hunan is located in the south of the Yangtze River, with low latitude, subtropical monsoon region, humid climate and obvious continental characteristics. Winter is often controlled by dry and cold air masses from Siberia and Mongolia Plateau, which is relatively dry and cold. Under the influence of quasi-static front and cyclone activity, it can bring some rain, snow and frost weather.

The warm and humid climate is the basic feature of Guangdong Province. In terms of climate types, most parts of Guangdong Province have a warm and humid subtropical monsoon climate, while the southwest Leizhou Peninsula has a tropical monsoon climate.

Guangxi is located in a low latitude area, bordering tropical oceans in the south, Nanling Mountains in the north and Yunnan-Guizhou Plateau in the west. There are many rivers in the territory and the geographical environment is complex. Under the combined action of solar radiation, atmospheric circulation and underlying surface, climate types have the following characteristics: (1) Climate types are diverse, with long summer and short winter. (2) Rain and heat resources are abundant and in the same season. (3) The climate is changeable and disastrous weather is frequent.

Hainan is the place with the most tropical marine climate characteristics in China. It is warm and hot all year round, with abundant rainfall, obvious dry and wet seasons, strong normal wind, frequent tropical storms and typhoons and diverse climate resources.

Chongqing is located in the subtropical inland area of the northern hemisphere, and its climate characteristics are just like several proverbs: unstable temperature in early spring, hot and rainy summer, cool and rainy autumn, warm and snowy winter.

Sichuan is located in the subtropical zone, and the climate is complex and diverse due to the complex topography and the alternating influence of different monsoon circulation. The eastern basin belongs to subtropical humid climate. Affected by topography, the western plateau is dominated by vertical climate zones, from southern mountains to northern plateau, from subtropical zone to sub-frigid zone, and there are various climate types from subtropical zone to permafrost zone vertically.

Guizhou Province is located in the subtropical East Asian continental monsoon region, and its climate type belongs to the humid monsoon climate of China subtropical plateau. The main climatic characteristics are: (1) Most parts of the province have mild climate, with no severe cold in winter, no intense heat in summer and distinct four seasons. (2) The annual rainfall is abundant and unevenly distributed in time and space. (3) Poor lighting conditions, rainy days and high relative humidity. (4) Our province is located in a mountainous area with low latitude, and the terrain height difference is wide, the weather and climate characteristics are quite different in the vertical direction, and the three-dimensional climate is obvious.

Yunnan's climate, first, the annual temperature difference is small and the daily temperature difference is large. Second, Yunnan is rich in precipitation, with clear wet and dry conditions and uneven distribution. Third, the vertical climate change in Yunnan is very obvious. Fourth, Yunnan has a long frost-free period.

The climate in Tibet is very different. Generally speaking, it belongs to the plateau continental monsoon climate, with a large temperature difference between day and night, but the sunshine time in winter is long and not cold.

Shaanxi has a mild climate.

Gansu province has a dry climate, large daily temperature difference, abundant sunshine and strong solar radiation.

The climate of Qinghai Province is characterized by cold and drought, which belongs to a typical continental plateau climate. 1. Leng Xia is cool in winter, and spring and autumn are connected. 2. The daily temperature difference is large and the annual temperature difference is small. 3. Drought and little rain.

Ningxia is located inland, far from the ocean, and on the western edge of China monsoon. Winter is controlled by Mongolian high pressure. Just as cold air moves southward, Xia Dong is at the western end of the southeast monsoon, forming a typical continental climate (continental degree 52 ~ 68), with long cold winter, short hot summer, fast warm spring and early cool autumn. Drought and little rain, abundant sunshine, strong evaporation, windy and sandy; It is cool in the south and warm in the north, wet in the south and dry in the north, and there are many meteorological disasters.

The climate in Xinjiang is characterized by drought, characterized by sufficient light and heat and scarce precipitation.

Hong Kong has a subtropical climate.

Macao is located in the south of the Tropic of Cancer, deeply influenced by the ocean and monsoon, and has a subtropical maritime climate, with no heat in summer and no cold in winter, and the trees in the city are evergreen all year round. The annual average temperature is 2 2.3 degrees Celsius, and the annual temperature difference is 65438 0.4 degrees Celsius, with a gentle change.

Taiwan Province has a tropical monsoon climate, with high temperature and rainy weather all year round and many typhoons in summer.