It is difficult to make any generalizations about China's climate. There are seven local climatic zones: northeastern, where summers are often damp and winters are frosty and harsh; the Central China zone where coastal areas are affected by tropical cyclones; tropical and subtropical zones of Southern China; the southwestern zone, where mountains moderate the summer heat; Tibetan Plateau, bordered by mountain ranges; deserts of Xinjiang; and finally, the Inner Mongolia zone, characterized by sharp seasonal temperature changes. In China, at any time of the year, temperatures can vary from -40° in winter in Inner Mongolia to +40° in hot summer in the south. Spring and autumn are perhaps the best times to travel, with many hotels becoming overcrowded due to the influx of tourists in the summer. Of course, the situation in different areas can vary significantly depending on local holidays.

China's climate is characterized primarily by monsoon rains and pronounced seasons, frequent northerly winds with little rainfall in winter and frequent southerly winds with heavy rainfall in summer. The variety of general climatic conditions includes cold air currents, cyclones, periodic rains and typhoons. Also characteristic is a pronounced continental climate with wide variations in temperature and precipitation, especially between the lower and higher limits. In winter, temperatures in China are lower than in other countries located at the same latitude; in summer they are much higher. For example, Huma County in Heilongjiang Province and suburban London are located between 51° and 52° north latitude. The average January temperature in Huma County is -27.8°C, and in London, where the vegetation remains green, as in Shanghai and Hangzhou, located between 30° and 31° north latitude, 3.7°C. Tianjin and Lisbon are located at 39° north latitude, but in Tianjin average temperature January -4.1°C, and the lowest is -22.9°C, while in Lisbon the average January temperature is 9.2°C, and the lowest is -1.7°C. Climatic conditions different regions of the country are very different from each other due to the vast territory of China and the complex structure of its surface.

The general picture of the distribution of annual precipitation in China is characterized by its progressive decrease from the southeastern coast (1000-2000 mm; a record figure was recorded in Hoshaoliao, Taiwan Province - 8408 mm) to the interior of the northwest (100-200 mm), others In other words, the further from the coast, the less precipitation. Eastern Xinjiang, located in the very center of the Eurasian continent, is the arid center of China with an annual rainfall of less than 50 mm, and here in the Turfan Depression, Toksun County, the average annual rainfall of only 3.9 mm is the least rainfall in the entire country.

Best time to visit:

Beijing In Beijing, each season has its own characteristics. Summer is hot and rainy, autumn is pleasant and cool, winter is cold and spring is dry. In January the average temperature is -5°C - -10°C in July +24°C - +26°C. The annual temperature difference is 15? - 30°C. The frost-free period lasts 6 and a half months (starting in April). The annual precipitation level is 500 - 700 mm. You can come to Beijing at any time of the year. Each of them is good in its own way. Pay attention to what happens in spring strong wind, and in summer the temperature reaches 30 degrees, but the autumn weather is pleasant and sunny.


Tianjin In Tianjin, the seasons differ significantly from each other. In January the average temperature is -4°C - 6°C in July - +26°C the most heat- +39.6°C. The frost-free temperature period lasts 6 and a half months (starting in April). The annual precipitation level is 500 - 700 mm, 70% of precipitation falls in summer. The city of Tianjin borders Beijing. In winter, temperatures in Tianjin are slightly higher than in Beijing. You can come to Tianjin at any time of the year, each of them is interesting in its own way. Meanwhile, we can safely say that autumn is the golden season for the traveler.

Hohhot Hohhot has a dry continental climate. Summer is short but relatively cool. The cold (winter) period lasts 6-7 months. The average temperature in January is -10°C in July - +20°C - +23°C. The daily temperature range is large, which is explained by the influence continental climate. The annual precipitation level is 300 - 400 mm. Hohhot is dry in winter and spring, and sandstorms are common. June, July, August and September are considered the best travel seasons. Keep in mind that daily temperature fluctuations reach 20 degrees, so you should stock up on warm clothes.

Jinan Jinan is located in a temperate monsoon climate zone. It is windy in spring, rainy in summer, sunny in autumn and dry in winter. In January the average temperature is -4°C and in July +28°C. The period of freezing of rivers and lakes lasts from the third ten days of December to the second ten days of February. You can come to Jinan at any time of the year, such as February, March, July, August and October to admire the famous Baotuquan Springs. The best months for climbing Mount Taishan are April, May, June, July, August, September, October and November. Meanwhile, the landscape will be beautiful and majestic even in winter, when there is snow on the mountains.

Shanghai In Shanghai, the seasons are different from each other. In summer it is humid and hot, in winter it is cold. In January the average temperature is +3°C and the most low temperature- -5 - 7°C in the hottest month - July - the average temperature is +27°C in July and August the highest temperature in May is +36°C - +37°C at one time the temperature reached +40.2°C . The frost-free period lasts 8 and a half months (starting from the end of March). The annual precipitation level is 1,100 mm. Between the second ten days of June and the first ten days of July it rains (during the ripening period of the mume plum) for 20 days. Typhoons and tropical downpours are common in July, August and September. You can come to Shanghai at any time of the year, but we recommend avoiding the rainy season (during the ripening period of the mume plum) and paying Special attention for storm warnings about possible typhoons.


Haikou Haikou is located in a tropical humid monsoon climate zone. The annual temperature range is less than 15°C. The city has a characteristic maritime climate. The coldest season is January and February, the average temperature is +17.2°C. The hottest months are July and August, the average temperature is +27°C. There is between 1,500 and 2,000 mm of precipitation per year. The best season to travel to Haikou is from November to May. The eastern part of Hainan Island is considered a "typhoon corridor", so special attention should be paid to storm warnings.

Wuhan Wuhan is located in the subtropical zone humid climate. The average temperature in January is +4°C and July is +28.8°C. The city of Wuhan is called a "stove", the period when the temperature exceeds +35°C lasts 22 days, then relative humidity reaches 70%. Wuhan, with its sultry climate, is one of the hottest places in our country. The daytime temperature range is imperceptible; at night it is also hot in Wuhan.

Huangshan Mountains The climate in the Huangshan Mountains is warm and humid. Seasons differ significantly from each other. In January, the average temperature is -3°C; the highest temperature is +0.6°C; the lowest temperature is -6.2°C. In July, the average temperature reaches +17.6°C; the highest temperature is +20.5°C; the lowest temperature is +15.3°C. You can come to the Huangshan Mountains at any time of the year. Every season in the Huangshan Mountains is beautiful and attractive in its own way. Please be aware of the temperature differences inherent in the mountains, so be prepared with warm clothing, especially during the snow season.

Harbin In Harbin, temperatures range from -22°C in January to +21°C in July. The annual precipitation level is 450-700 mm, in summer up to 60% of its annual volume falls. You can come to Harbin at any time of the year. The best seasons are December-January and July-September. In winter, tourists can admire the main decoration of Harbin - snow, and in summer it is pleasant and cool here. Harbin - wonderful place summer holiday.

Urumqi Urumqi is the most distant city from the sea in the world, located in an arid area where it rarely rains. The climate of Urumqi is distinctly continental. The annual temperature ranges from -15°C in January to +25.7°C in July-August. Annual precipitation is 194 mm. Spring and autumn are short, and summer and winter are long, with a significant daily temperature range. The best season to travel to Urumqi is June-October; this is a time of pleasant temperatures, a riot of flowers and ripening fruits. When traveling to Urumqi in early spring and in the fall, don’t forget to bring warm clothes with you.

Yinchuan In Yinchuan, every season is good in its own way. Winter is long and harsh, summer is short. It rarely rains. There are significant daily temperature fluctuations. The sun shines 3,000 hours a year. Temperatures range from -8°C in January to +22°C in July. The frost-free period lasts 5 and a half months. The annual precipitation level is 700 mm, and in summer up to 60% of its total falls. The climate in Yinchuan is typically continental - dry, with rare rainfall and frequent dust storms. The best season for travel is May-October. Therefore, in May-August, prepare summer clothes, and in September and October, prepare warm clothes.

Xining In the city of Xining, the amplitude of daily temperature fluctuations is large, and the amplitude of annual temperature fluctuations is small. The average temperature is from -15°C in January to +16°C in July. The frost-free period lasts 6 and a half months, the annual precipitation level is 400 mm. It is preferable to come to Xining in spring, summer and autumn. Summer in general - best season for traveling. Due to excellent weather conditions in summer, Xining - perfect place for relax. In summer, in the area located 150 km west of Xining Lake. Qinghai average daily temperature is +10°C; midday temperatures reach +22°C; night temperatures in July drop to +2°C. Travelers suffering from cardiovascular diseases should keep in mind that Xining is located at an altitude of 3,200 m above sea level, which explains the 20% lack of oxygen. In spring and autumn, be prepared with suitable clothing to protect you from the cold.

Lanzhou Lanzhou is located in the mainland "heart" of China. Due to its geographical location (the city is located in a basin surrounded by mountains), a unique climate with cool summer and warm winter. The annual temperature ranges from -6.9°C in January to +22.2°C in July. The lowest temperature is from -13°C to -16°C. In July and August the highest average temperature reaches +29.2°C. The tallest average monthly temperature in autumn - +22.1°C and the lowest - 10.7°C. The average monthly temperature in winter ranges from 0°C to -8.2°C. The annual precipitation level is 328 mm. The frost-free period lasts 179 days. You can visit Lanzhou at any time of the year. The best season is March-September, but do not forget about significant daily temperature fluctuations. During cold seasons, be sure to bring warm clothes with you.

Lhasa Lhasa is located at an altitude of 3,700 m above sea level. Thin air, rare rains, frequent winds and a large number of sunny days- these are characteristics climate of the area in which Lhasa is located. It's not frosty in winter, not hot in summer. The average temperature ranges from -4°C in January to +15°C in July. Daily temperature fluctuations are quite significant. The frost-free period lasts 2 and a half months, starting in July. Due to the fact that Lhasa is located high above sea level, the oxygen content in the air is 62%-65.4% of the norm on the plain. Persons suffering from diseases of the cardiovascular system and hypertension should refrain from traveling to the administrative center of the Tibet Autonomous Region. The "golden season" for traveling in Tibet is March-October. Temperature and humidity in summer are better than other times of the year. Always carry warm clothing and sunscreen with you.

Chongqing Chongqing is warm in winter and hot in summer. The coolest month is January, when the average temperature reaches +5°C. It's stuffy in the summer. The hottest month is July, the average monthly temperature is +29°C. At one time, the highest temperature reached +44°C. Therefore, Chongqing is called one of the "three furnaces" located in the Yangtze basin. The frost-free period lasts for more than 10 months, starting in February. The level of annual precipitation reaches 1,100 - 1,300 mm. IN river valley Fogs are common in winter and spring, which is why Chongqing is called the “city of fogs.” The foggy period lasts more than 100 days, sometimes reaching 200 days. Spring, autumn and winter are the best seasons to travel to Chongqing. We do not recommend coming there at the height of summer.

Kunming In Kunming, every season is as beautiful as spring. The average temperature ranges from +10°C in January to +21°C - +25°C in July. The frost-free period lasts 11 months, starting in February. Daily temperature fluctuations reach 8°C - 10°C; annual precipitation is 1,000 - 1,500 mm; the period from May to October accounts for 85%-90% of the annual volume. There are no significant differences between the seasons in Kunming, but there is a big difference between the dry and wet seasons. The weather in January and February is mild; in the third ten days of July, the torch festival is celebrated by the Yians, Bai and Mongols. During this time, tourists can admire the beauty of the Stone Forest near Kunming and watch how ethnic minorities celebrate their holiday. Most parts of China experience hot weather in July and August, and Kunming experiences between 20°C and 25°C during this time, so no one will regret spending the summer in Kunming.

Chengdu In Chengdu early spring, long summer and warm winter. Temperatures range from +6°C in January to +25°C in July. The frost-free period lasts 8-10 months. and usually begins in the first ten days of January - early March. The annual precipitation level is 1,500 mm. You can come to Chengdu at any time of the city, but it is better to visit out-of-town attractions during the most suitable seasons. So, it is best to come to the Jiuzhaigou Nature Reserve in late spring and early autumn, i.e. in September and October. In spring it is a little cool and, in general, quite unstable temperatures. The average temperature ranges from +9°C - +18°C in January to +19°C - +22°C in summer. The rainy season occurs in July and August, so care should be taken to protect yourself from rain. In autumn the weather is clear, the average daily air temperature is +7°C - +18°C; however, daily temperature fluctuations are significant. The Emeishan Mountains experience altitudinal temperature changes. In areas located halfway to the summit, temperatures are 4°C - 5°C lower than in the foothills, and at the peaks - 10°C lower. The best seasons to travel to the Sigongyang Mountains in the Ganzi region are December, January, February and May. In December and January the average temperature reaches -2°C, in July and August +12°C and in May and October there is frequent rain.

Guiyang Guiyang is located in a subtropical humid monsoon climate, with characteristically warm winters and cool summers. Temperatures range from +5°C in July to +25°C. The frost-free period lasts 8 - 10 months (it begins in the second ten days of February - early March). The annual precipitation level is 1,400 mm. You can come to Guiyang at any time of the year. The best season to visit Huangoshu Waterfall is summer or autumn. You will be able to enjoy the magnificent scenery and view of a waterfall 67 m high and 84 m wide (in its upper part). They say about Guizhou province: “You won’t find three in a row here.” square meters The surface is flat and there are never 3 clear days in a row." At night it is often rainy, but during the day it is clear. We recommend taking warm clothes with you and taking care of protection from the rain.

Xiamen Xiamen has a subtropical maritime climate. Temperatures range from 4°C to 20.9°C heat. The hottest month of the year is August, the average monthly temperature is +28.2°C and the highest temperature in August is +36.4°C. Xiamen is very favorable weather, you can come here at any time of the year. Pay special attention to warning signals for an approaching typhoon. Sanya The city of Sanya is located in the southern part of the island. Hainan. The average temperature in January is +20.9°C. The hottest months are July and August, when the average monthly temperature reaches 29°C. It can be argued that it is eternal summer in this city. If possible, try to avoid visiting the island during high summer. Golden season - November-May. Hainan is traditionally considered a “typhoon corridor”, so we advise you to always pay special attention to storm warnings from meteorologists.

Dali The average annual temperature in Dali is +15.1°C in January - the coldest month - the average temperature is +8.7°C and in July - the hottest - +20.1°C. The annual precipitation level is 1078.9 mm. The climate is characterized by moderate winters and cool summers. You can visit Dali at any time of the year, especially in July and August - thanks to the peculiar climate of this city, you will be able to avoid the summer heat.

Hainan Hainan is located at the same latitude as Hawaii, so the island is often called “East Hawaii”. The island is washed by the waters of the South China Sea, the average annual air temperature is +24°C, water temperature is +26°C. The sun shines 2563 hours a year, there is no winter and eternal summer reigns, the amount of precipitation per year is 1279 mm, during the rainy season here from August to September it occurs irregularly, with interruptions. If we talk about Hainan, then best time The months to visit the resort are September to November and February to May. The average daily air temperature in November is +26…28°C, water temperature is +25°C.



Climate of China

China's climate is characterized primarily by monsoon rains and pronounced seasons, frequent northerly winds with little rainfall in winter and frequent southerly winds with heavy rainfall in summer. The variety of general climatic conditions includes cold air currents, cyclones, periodic rains and typhoons. Also characteristic is a pronounced continental climate with wide variations in temperature and precipitation, especially between the lower and higher limits. In winter, temperatures in China are lower than in other countries located at the same latitude; in summer they are much higher. For example, Huma County in Heilongjiang Province and suburban London are located between 51° and 52° north latitude. The average January temperature in Huma County is -27.8°C, and in London, where the vegetation remains green, as in Shanghai and Hangzhou, located between 30° and 31° north latitude, 3.7°C. Tianjin and Lisbon are located at 39° north latitude, but Tianjin has an average January temperature of -4.1°C and the lowest is -22.9°C, while Lisbon has an average January temperature of 9.2°C and the lowest low -1.7 C. The climatic conditions of different regions of the country differ greatly from each other due to the vast territory of China and the complex structure of its surface. In 1958, the Geographical Regionalization Committee of the Chinese Academy of Sciences divided the country into six climate zones (not including the Qinghai-Tibetan Plateau).

The general picture of the distribution of annual precipitation in China is characterized by its progressive decrease from the southeastern coast (1000-2000 mm; a record figure was recorded in Hoshaoliao, Taiwan Province - 8408 mm) to the interior of the northwest (100-200 mm), others In other words, the further from the coast, the less precipitation. Eastern Xinjiang, located in the very center of the Eurasian continent, is the arid center of China with an annual rainfall of less than 50 mm, and here in the Turfan Depression, Toksun County, the average annual rainfall of only 3.9 mm is the least rainfall in the entire country. In 1958, taking as a basis the aridity index (the ratio of precipitation to possible evaporation) on days with an average daily temperature of ≥10°C, the Geographical Regionalization Committee of the Chinese Academy of Sciences divided the country from southeast to northwest (including Qinghai-Tibet highlands) into the following four areas:

Humid region (32.2% of the country's territory). Aridity less than 1.0, annual precipitation more than 750 mm, forest vegetation.

Semi-humid area
(14.5% of the territory). Aridity from 1.0 to 1.5, annual precipitation from 400 to 750 mm, vegetation of forests and meadows.

Semi-arid region
(21.7% of the territory). Aridity from 1.5 to 2.0, annual precipitation from 200 to 400 mm, steppe vegetation.

Arid region
(30.8% of the territory). Aridity more than 2.0, annual precipitation less than 200 mm, vegetation of desert steppes (aridity from 2.0 to 4.0) and deserts (aridity more than 4.0).

Geographical features

China is a country located in East Asia. The Pacific Seas - South China, East China, Yellow - wash China from the east. The sea coast stretches for 14.5 thousand km from the north (North Korea) to the south (Vietnam). The island of Taiwan is separated from the mainland by the Taiwan Strait.

The country has land borders with: Mongolia (in the north); Russia and North Korea(in the north-east); Russia and Kazakhstan (in the northwest); Afghanistan, Tajikistan, Kyrgyzstan (in the west); India, Gilgit-Baltistan, Bhutan and Nepal (in the southwest); Laos, Myanmar, Vietnam (in the south).

Note 1

The total area of ​​the country is 9.6 million square meters. km. China is one of the four largest countries world, which also includes Russia, the USA and Canada.

China has a variety of terrain: mountains, depressions, plateaus, vast plains and deserts.

Major orographic regions include:

  1. Tibetan Plateau. Located in the southwest of the country, the altitude is more than 4000 m above sea level.
  2. The belt of high plains and mountains is the northern regions of the country. The mountains of Central China and Sichuan, with altitudes from 1500 to 3000 m. There is a change in natural zones - from cold high-mountain deserts to subtropical forest.
  3. Low accumulative plains and low mountains. They occupy the east, northeast and south of the country. Altitude – less than 1500 m above sea level.
  4. From north to south from Beijing to Shanghai, the Great Chinese Plain, the Yangtze Delta and the Yellow River Valley stretch along the sea coast.
  5. The basin of the Pearl River and its tributary Xijiang is located in the southern part of China. The Wuyi Range and the Nanling Mountains separate it from the Yangtze River basin.

Climate zones

The climate of China varies from subtropical (southeastern regions) to arid or sharply continental in the northwest.

The weather of the southern coast is determined by monsoons, which are formed as a result of the interaction of the absorption properties of the ocean and land.

Seasonal movements of air masses contain a lot of moisture in the summer, and are relatively dry in the winter. The appearance and disappearance of monsoons largely determine total precipitation throughout the country.

Most of China's territory lies in the temperate climate region. However, the peculiarities of the relief and geographical location of the country relative to the Pacific Ocean determine a wide range of meteorological and temperature regimes.

The following climate zones are distinguished in China:

  • Temperate climate. Characteristic of the northern territory of China, represented by the province of Heilongjiang and the western regions.
  • Sub tropical climate. South-eastern regions and central regions.
  • Tropical monsoon climate. South coast, Hainan Island.
  • Sharply continental climate. Northwestern regions.

In China, there are several climatic zones characterized by varied topography and climate: coastal areas, mountain ranges, deserts, islands. Characterized by large fluctuations in average temperatures between the northern, central and southern regions, high humidity in summer in many central and southern territories.

Natural areas

In China there are three major natural areas:

  1. Eastern Monsoon Region;
  2. Cold Alpine Qinghai-Tibet Region;
  3. Northwestern arid region.

The eastern monsoon region occupies mainly the coast of the South China and East China Seas. It is the warmest and most humid area in summer in China. Summer is long, but not very hot. Winters are mild and cool; in January the temperature rarely drops below +10 ºС. There is heavy rainfall throughout the year. In the tropical southeast, the rainy season runs from May to October. During the summer, the region is subject to frequent typhoons and floods.

Climate in Tibet Autonomous Okrug and in Qinghai province it is extremely harsh, cold alpine. Practically all year round the temperature does not rise above 0 ºС. Piercing winds are blowing. The landscape of this region was determined by: cold, rocky and poor soils, low humidity. Most of the territory is steppe, desert and semi-desert. In low-lying gorges there are small forest strips.

The climate of the southeastern regions of the Tibetan Plateau is somewhat milder, since Indian Ocean come warm air masses.

The northwest territories are characterized by a desert, dry climate with significant fluctuations in daily and seasonal temperatures. Warm air from the southeast of the country over the mountain plateaus and cold plains of the northwest quickly cools and turns into anticyclones, predetermining clear, dry weather with very hot summers and exceptionally frosty weather in winter. Precipitation is scanty and falls mainly in late spring - early summer. Most of the territory is steppe and desert. The climate softens somewhat closer to central regions. The most favorable climate is in the Yangtze River basin. The southeast monsoons reach here, summers are warm and winters are moderate.

Climatic features

In Heilongjiang, the average temperature in winter is -16 ºC, sometimes dropping to -38 ºC. The average July temperature is +20 ºС. In the south of Guangdong province, the average temperature in winter and summer is +10 ºС and +28 ºС, respectively.

Different regions of the country receive different quantity precipitation. On the southern slopes of Qinling, precipitation is abundant, and its maximum is observed in the summer during the monsoon period. To the north and west of the mountains, the amount of precipitation decreases. The driest areas are the northwestern regions. Here are the Ordos, Gobi, and Taklamakan deserts.

The rainy season lasts from May to September. More than 6,000 mm of precipitation may fall during this period alone. In summer from the Indian and Pacific Oceans Monsoon winds are formed, which determine the amount of precipitation. In the provinces in the south of the country (Hainan, Guangdong, Guangxi), the rainy season opens with the monsoons. Rainy weather in June-August moves to the northern regions.

The eastern and southern regions of China are characterized by typhoons, monsoons, tsunamis, floods, and droughts.

Every year in the spring, yellow dust storms are observed in the northern regions, originating in the northern deserts and heading towards Japan and Korea.

Natural areas of China are very diverse, and this is due to the impressive size of the country’s territory and its geographical location. In one square, such natural complexes such as taiga, steppes and forest-steppes, monsoon and variable rain forests, evergreen hard-leaved forests and areas of altitudinal zonation.

Climate

The climatic features of China are determined by two factors:

  • large latitudinal extent;
  • distance from the sea.

The main regions are located in the temperate climate zone, with a tropical climate prevailing in the south and a monsoon climate on the coast.

In the south, the temperature difference is about 20 Celsius; in the north, temperature fluctuations throughout the year are even more noticeable. The coldest province is Heilongjiang - temperatures in the winter months can drop to -30 degrees.

Rice. 1. The nature of China is very diverse

The difference in precipitation is even higher than in air temperature. However, it no longer depends on latitude, but on distance from the sea. The wettest region of the country is the southeast, where monsoon showers occur endlessly in the summer. The driest part of China is the northwest, where the Gobi, Ordos and Taklimakan deserts are located.

Soils

China's soils are changing along with natural areas. In the northeast, meadow soils predominate, and the north-west of the country is covered with gray soils, gray-brown, mountain-steppe soil types. Black soil is found on the coast of the Songhua River. Red soils predominate on the plains.

A big problem of local soils is their salinity, which is largely due to the arid climate. On the coast of the Yellow Sea, soil salinization depends on the close proximity to the sea. Agriculture in these regions is possible only after the salts have been washed away.

Human activity also poses a serious threat. Active deforestation and uncontrolled grazing of livestock have caused large areas of land to lose their fertility and become deserted.

Flora

In the northeast there are taiga forests consisting of Korean cedar and larch. As you move south, they are replaced by broad-leaved forests, dominated by oak, walnut, maple, and linden.

In the center there are subtropical forests of camellias, magnolias and laurel trees. The south of China is occupied by the tropics, and in the west there is a zone of savannas and woodlands.

💡

The most common plant in China is bamboo, represented by 35 species. Being the fastest growing plant on Earth, it is able to regenerate in as soon as possible. Bamboo is used in various industries: food, construction, manufacturing.

Rice. 2. Bamboo

The flora of China is very diverse, but due to unreasonable use natural resources there are almost no rich people left on the plains forest areas, which only partially survived in the mountainous regions of the country.

Fauna

The northeast is home to hares, wolves, foxes, wild boars, lynxes and raccoons. In the north-west there are typical representatives of steppes and deserts: marmots, ground squirrels, jerboas, goitered gazelles, steppe wolves.

In the mountains you can find such highland inhabitants as the Tibetan bear, red wolf, lynx, wild yak, mountain goat, and orongo antelope.

Rice. 3. Red wolf

Representatives of the tropics live in the south: leopards, golden monkeys, palm martens, giant squirrels.

What have we learned?

In China, natural areas are very diverse and very well defined. They replace each other both in latitude and with distance from the sea. This diversity was made possible thanks to large area occupied by China.

Evaluation of the report

average rating: 3.2. Total ratings received: 17.

China is a huge state located in several natural zones. Due to the peculiarities of its geographical location and topography, the climate of China is extremely heterogeneous. While in one province the inhabitants suffer from the cold, in another the population enjoys the tropical heat.

Researchers distinguish here 3 large natural areas, each of which can also be divided into subzones:

  • Eastern Monsoon Region;
  • Cold Alpine Qinghai-Tibet Region;
  • Northwestern arid region.

Eastern Monsoon Region

This region, which occupies mainly the coast of the East China Sea and the South China Sea, is the wettest and warmest in China. In summer, streams of well-heated air rush from the sea to the coast, bringing with it showers and thunderstorms. These winds determine the specifics of the local climate.

Southern China can be described as subtropical zone. Summer here is very long, but not too hot. Winter is quite mild, slightly cooler than summer: the average January temperature rarely drops below +10°C. At the same time, heavy rainfall occurs throughout the year. Exactly climatic features this region made it especially attractive to farmers. Since ancient times, it has successfully developed on the southern coasts Agriculture. Climatically, the southern part of China is considered one of the most favorable regions on the planet.

The situation is slightly different in the tropical southeast. The rainy season here falls from May to October. It is extremely unsafe to be here in the summer, since it is at this time that the area is subject to frequent floods and typhoons. The last such disaster, which occurred in August 2017, claimed the lives of 16 people.

Cold Alpine Qinghai-Tibet Region

When assessing the Chinese climate, the rule is: the further west you are from the sea coast, the less precipitation. Wet monsoons simply do not reach the western part of the country, where Qinghai province and the Tibet Autonomous Region are located.

The climate here is extremely harsh: for approximately 10-11 months a year the temperature does not rise above zero, and piercing icy winds accelerate the evaporation of moisture from the soil. Cold weather, poor, rocky soils and low humidity defined the landscape of this region. Most of Tibet and Qinghai are deserts, semi-deserts and steppes in which only the hardiest plants survive. Forest belts are found only in low-lying gorges. Mostly cold-resistant oaks, maples and conifers grow here.

The climate in the southeast of the Tibetan Plateau is slightly milder, since warm air currents from the Indian Ocean often penetrate here in the summer.

Northwestern arid region

The term "arid" climatologists designate a dry, desert climate with large fluctuations in daily and annual temperatures. This concept best characterizes the climate of northwestern China. Usually warm air from the southeast of the country it gradually moves to the northwest into the territory of Inner Mongolia. Above these cold plains and mountain plateaus, air masses quickly cool, sink down and turn into anticyclones. Due to anticyclones, northwestern China experiences mostly dry, clear weather with very hot summers, during which dust storms often occur, and extremely frosty winter. Scanty precipitation occurs only in late spring and early summer.

Most of the territory of northwestern China is occupied by steppes and deserts, sometimes completely devoid of vegetation. However, the formation of severe natural conditions This region was associated not only with its geographical location, but also with the barbaric activities of man himself. Southern Inner Mongolia was once home to broadleaf forests, but they were all cut down, disrupting the region's fragile ecosystem and hastening its transformation into a lifeless desert.