What are the climate types on the earth, and what are the characteristics of each climate type?
What are the climate types on Earth and the characteristics of each climate type?
Tropical rainforest climate - high temperature and rain all year round
Perennially affected by the equatorial low pressure belt
Near the equator, between 10 degrees north and south latitude
Tropical grassland climate - divided into dry and wet seasons
Alternately controlled by the equatorial low pressure belt and subtropical high pressure
10-20 degrees north and south latitude, west coast of the continent
Tropical Desert climate - hot and dry all year round
Affected by the subtropical high all year round
20-30 degrees north and south latitude, west coast of the mainland
Mediterranean climate - hot and dry in summer, Mild and rainy in winter
Controlled alternately by the westerly belt and subtropical high pressure
30-40 degrees north and south latitude, west coast of the continent
Temperate maritime climate - mild and rainy all year round
Affected by the westerly belt all year round (the warming and humidifying effect of warm currents)
40-60 degrees north and south latitude, west coast of the mainland
Tropical monsoon climate - high temperature and rainy summer , high temperature and little rain in winter, divided into two seasons: rain and dry season
Differences in thermal properties of land and sea, (the cause of the south subtropical monsoon plus the seasonal movement of pressure belts and wind belts)
North and south latitude 15 -25 degrees, east coast of the mainland
Subtropical monsoon climate - high temperature and rain in summer, mild and less rain in winter
Differences in thermal properties between sea and land
25-35 degrees north and south latitude, mainland East Coast
Temperate monsoon climate - hot and rainy in summer, cold and dry in winter
Differences in thermal properties between sea and land (monsoon in southwest my country, coupled with the influence of terrain)
South 35-55 degrees north latitude, east coast of the continent
Temperate continental climate - mild and rainless summers, cold and dry winters
Inside the temperate continent, far away from the ocean
Polar climate -Low temperature all year round with little precipitation
It is divided into tundra zone and ice sheet zone. The tundra zone is mainly along the Arctic Ocean; the ice sheet zone is on the Antarctic continent and Greenland
Mountain climate - as the altitude increases, the temperature decreases and precipitation changes. Characteristics of each climate type
1. Tropical rainforest climate is mainly distributed near the equator, such as the Malay Islands, Amazon Plain, Congo Basin and the Gulf of Guinea coast. It is characterized by high temperatures and rain all year round, with small annual temperature ranges, and the average monthly temperature is between 25-28°C. , the annual precipitation is mostly above 2000 mm, and the distribution is relatively even throughout the year.
2. Tropical grassland climate is mainly distributed in the north and south sides of the tropical rainforest climate zone. The average annual temperature here is high, but the annual temperature range is slightly greater than that of the tropical rainforest climate. The annual precipitation is mostly between 400-1500 mm, and there are obvious dry and wet seasons. , the further away from the equator, the longer the dry season and therefore the less precipitation.
3. Tropical monsoon climate is distributed in South Asia and Indochina. It is characterized by high temperatures throughout the year. The average temperature of the coldest month is also above 18°C. Precipitation is closely related to wind direction. Northeasterly winds from the mainland prevail in winter and there is little precipitation. In summer, prevailing winds from The southwesterly winds of the Indian Ocean bring abundant precipitation. The annual precipitation in most areas is 1500-2000 mm, but in some areas it is much more than this.
4. Tropical desert climate is distributed in the interior of the continent or the west coast of the continent near the Tropic of Cancer. It is characterized by high annual average temperature, large annual temperature difference, larger daily temperature difference, and scarce precipitation. The annual precipitation is generally less than 250 mm, and in many areas there is only a few dozen Millimeters or even several millimeters, precipitation variability is very large, and it often does not rain for several consecutive years.
5. The subtropical monsoon climate is distributed in the subtropical area on the east coast of the mainland. The winter here is not cold, the average temperature in January is generally above 0°C, and the summer is hot. The average temperature in July is generally around 25°C. The wind direction changes significantly in winter and summer, and the annual precipitation is average. Above 1000 mm, it is mainly concentrated in summer and less in winter. This type of climate is most typical in southeastern my country. In other areas, because there is a considerable amount of precipitation in winter, there is not much difference between dryness and wetness in winter and summer, so it is called a subtropical monsoon humid climate.
6. The Mediterranean climate is distributed in the subtropical areas on the west coast of the continent, with the Mediterranean coastal areas being the most typical, hence the name. This type of climate is characterized by mild winters, hot or warm summers, precipitation is mainly concentrated in winter, and dry summers, so it is also called a subtropical summer-dry climate.
7. The temperate maritime climate is distributed in the temperate zone on the west coast of the mainland. It is characterized by not being cold in winter (the average temperature in January is above 0℃), not hot in summer (the average temperature in July is below 22℃), and there is precipitation all year round. Precipitation is generally around 1,000 mm, and can reach 2,000 mm or more in places with favorable terrain.
8. The temperate monsoon climate is distributed in the eastern areas north of the Qinling Mountains and the Huaihe River in my country, the northern parts of Korea and Japan, and the eastern coastal areas of Siberia. It is characterized by warm summers and cold winters, with an annual precipitation of 500-1000 mm, mainly concentrated in summer, winter and summer. The temperature difference increases from south to north, and the precipitation decreases from south to north.
9. The temperate continental climate is distributed within the Eurasian continent and the North American continent. Due to the control of continental air masses throughout the year, the winters are cold and the summers are hot. The annual temperature range is large and the precipitation is less. The annual precipitation is less than 500 mm, forming a dry environment in the central part of the continent. Or a semi-arid climate; while in the northern part of the continent, due to the high latitude, cold and long winters, cool and short summers, low evaporation, and little precipitation, it is not dry, forming a special subarctic coniferous forest climate.
10． Polar climates are distributed in the northern edge areas of Eurasia and North America, Greenland, the Arctic Ocean islands and Antarctica. In the continental margins, winters are long and cold, but the average temperature in the hottest month in summer can reach 10°C. Moss and lichens are typical plants here, so it is also called a tundra climate; most of Greenland, the Arctic Ocean islands and Antarctica and other places The area is covered with ice and snow all year round, and the hottest monthly average temperature does not exceed 0°C, so it is called an ice sheet climate.
11. Alpine climate may occur at any latitude. It is characterized by vertical changes in temperature and precipitation. Temperature decreases with increasing altitude. Precipitation increases with increasing altitude within a certain altitude range. Above this altitude, it decreases with increasing altitude. . Earth's various climate types and their characteristics
Introduction
Tropical climate types
Subtropical climate types
Temperate climate types
Cold zone climate type
Alpine and plateau climate
Distribution of global climate types Climate type
[Edit this paragraph] Introduction< /p>
Cold, hot, dry, and wet conditions vary widely around the world, forming unique climate types. The climate of a place is the average weather condition for many years, and generally does not change much. The global climate can be roughly It is divided into 13 types, namely tropical rainforest climate, tropical grassland climate, tropical monsoon climate, tropical desert climate, subtropical desert steppe climate, subtropical monsoon humid climate, subtropical Mediterranean climate, temperate maritime climate, temperate monsoon climate, temperate continental climate Climate, frigid tundra climate, frigid ice sheet climate and alpine plateau climate.
[Edit this paragraph] Tropical climate type
Tropical rainforest climate
Also known as " Equatorial rainy climate”. Distributed between 5° and 10° north and south latitude on both sides of the equator. It is hot and rainy all year round, with the average monthly temperature ranging from 25 to 28°C, and the annual precipitation can reach more than 2,000 mm. The seasons are evenly distributed and there are no dry periods. Mainly found in the Amazon Plain of South America, the Congo Basin and the Gulf of Guinea coast of Africa, most of the Malay Islands in Asia and the southern part of the Malay Peninsula. Mainly distributed in the Amazon River Basin in South America, the Congo River Basin in Africa, the Gulf of Guinea, the southwest coast of the Indian Peninsula in Asia, the Malay Peninsula, the west coast of Indochina, the Philippine Islands and Irian Island, and Oceania from Sumatra to New Guinea.
Mainly affected by latitude factors:
1. Solar radiation: The amount of solar radiation is in the range of 100-180 kcal/cm*year. It makes for high temperatures all year round. Areas with stronger solar radiation will become deserts.
2. Atmospheric circulation: In the equatorial low-pressure zone, the trade winds gather near the equator, converge and rise, and the water vapor contained in them can easily form clouds and cause rain.
3. Influence of land and sea. Tropical rainforest climate locations are close to the sea or in large river basins, which provide abundant rainfall and small temperature differences. The terrain is low and suitable for rainforest growth.
4. Vegetation affects the strong transpiration of trees, making the environment more humid.
Tropical savanna climate
It is also called tropical dry and wet season climate, Savannah climate, tropical savanna climate, and tropical sparse steppe climate. They are roughly distributed between 10° north and south latitude and the Tropic of Cancer, typically in central Africa, most of Brazil in South America, and the northern and eastern parts of the Australian continent. The distribution area of this type is in the area controlled alternately by the equatorial low pressure belt and the trade wind belt. The temperature is high throughout the year, with the average annual temperature being about 25°C. When the equatorial low pressure belt is controlled, the equatorial air mass prevails and precipitation is concentrated; when the trade wind belt is controlled, the tropical continental air mass is controlled, resulting in drought and less rain. The annual precipitation is generally 700--1000 mm, and there is an obvious long dry season. The natural vegetation is tropical savannah.
The characteristics of the savanna climate are: when controlled by the equatorial low pressure belt, a wet season is formed; when controlled by the trade winds, a dry season is formed. Its distribution pattern is between 10° north and south latitude and the Tropic of Cancer. Students will have questions about this: "The moving range of the equatorial low pressure belt is within 10° north and south latitude. How does it control the climate of the savanna?" Through analysis, we can summarize the causes of this climate as:
? 1. Monsoon type
In midsummer, at low latitudes (especially on the continent), an equatorial westerly circulation is often inserted in the trade wind belts of the northern and southern hemispheres. It is formed, on the one hand, due to the seasonal movement of the planetary wind belt; on the other hand, it is due to the heating of the continents, which further encourages the equatorial low pressure trough to be strengthened on the continents when it moves.
In Northern Hemisphere summer time (July), the southeast trade winds in the Southern Hemisphere deflect to the north across the equator and deflect to the right, forming the southwest monsoon; in Southern Hemisphere summer time (January), the northeast trade winds in the Northern Hemisphere deflect to the south across the equator and deflect to the left. , forming the northwest monsoon. This phenomenon is most significant in the area from Africa through the Indian Ocean to the western Pacific.
1. Africa 10°N to 20°N and southern North America
? In summer, the two places are affected by the warm and humid southwest monsoon that passes over the warm current and is affected by the terrain uplift. control; and due to the convergence and rise of the southwest monsoon and the northeast trade wind, there is more convective rain and abundant precipitation, forming a wet season. In winter, it is controlled by a single, dry northeasterly trade wind, forming a dry season.
2. Africa’s 10°S to 20°S region and northern Australia
? In summer, the two places are controlled by the warm and humid northwest monsoon, and due to the divergence between the northwest monsoon and the southeast trade wind Together they rise, with more convective rain and abundant precipitation, forming a wet season. In winter, it is controlled by a single, dry southeasterly trade wind, forming a dry season.
2. Tropical front type
In summer, in the vast eastern tropical Pacific, the equatorial westerly wind is not significant, and due to the obstruction of the tall Andes Mountains, the warm and humid monsoon from the Pacific has South America's savanna climate zone has little impact. However, the southwest monsoon and northwest monsoon coming from the land converge and rise with the northeast trade wind and southeast trade wind coming from the tropical Atlantic and passing over the warm current, forming a tropical front with a lot of convective rain and a humid and hot climate.
The Guyana Plateau, Orinoco River Basin and northern Colombia north of the equator are humid and rainy from June to October; the interior of the Brazilian Plateau south of the equator is wet and rainy from October to March of the following year. Precipitation is abundant, forming a wet season. In winter, the two places are controlled by a single northeast trade wind and southeast trade wind respectively, resulting in dryness and little rain, forming a dry season.
3. Subtropical High Type
1. Southern South African Plateau (20°S to 30°S)
January is summer in the southern hemisphere, and formations occur within the continent. The wide-ranging thermal low pressure and the warm and humid southeast trade winds passing over the warm current blow toward the mainland, bringing more precipitation to the South African plateau, forming a wet season.
July is winter in the southern hemisphere, and the average altitude of the South African Plateau is above 1,000 meters. Due to the high terrain and lower temperatures, high pressure forms in the southern part of the continent and is connected with the maritime high pressure in the east. Due to the control of the subtropical high pressure zone, downdrafts prevail. Coupled with the existence of high pressure on land, the influence of trade winds from the ocean decreases, forming a dry season.
2. Southern Australia (30°S to 32°S)
Due to the seasonal movement of global pressure belts and wind belts, in summer (January), this area is affected by the southward moving Controlled by the subtropical high, downdrafts prevail, making it dry and less rainy, forming a dry season; in winter (July), controlled by the humid westerly wind moving north, forming a wet season.
4. Vertical zonal type
Areas near the equator on the East African Plateau
This area has an altitude of more than 3,000 meters. Due to the high terrain, the area has changed The temperature and precipitation conditions are so warm that a tropical rain forest climate cannot be formed. In summer, affected by the warm and moist southeasterly trade winds from the Indian Ocean that pass over the warm currents, precipitation is relatively heavy, forming a wet season. In winter, controlled by a single, dry trade wind, precipitation is low and ground evaporation is strong, forming a dry season.
5. Leeward Slope Type
The western part of the Great Dividing Range of Australia and the western part of Madagascar
The two places are located on the leeward slopes of the southeast trade wind and are affected by the subtropical high Control, the precipitation is less, but the dry and wet seasons are obvious, forming a savanna climate.
In summary, in summer, the savannah climate zone between 10° north and south latitude and the Tropic of Cancer is affected to a certain extent by the equatorial convergence zone. The location of this zone is generally The location of the equatorial low pressure belt, therefore, can also be said to be controlled by the equatorial low pressure belt.
Tropical desert climate
Tropical desert climate is mainly distributed in the inland areas where the Tropic of Cancer passes and the west coast of the continent. The Sahara Desert in northern Africa is the most extensive.
1. Precipitation is small but highly variable: Asvin in the Sahara Desert of North Africa once had no rain for many years; while Arica in the desert of northern Chile in South America had only rain for seventeen consecutive years. There were three measurable showers, and the total amount of the three showers was only 0.51 centimeters, which is very little precipitation. Iquigue, also located in the desert of northern Chile, had no rain for four consecutive years, but a shower in the fifth year dropped 15 centimeters. In another year, a shower recorded a rainfall of 63.5 centimeters, which shows the great variability. Rainfall in tropical deserts is mostly explosive showers, often causing severe soil erosion.
2. High temperature and large temperature difference: Due to low cloud cover, strong sunshine, lack of vegetation coverage, and low air humidity, the temperature rises very quickly during the day. There has been a record of as high as 58℃ in North Africa. Generally speaking, the monthly average temperature in summer is between 30℃~35℃, and the high temperature lasts for a long time. For example, in Aden on the Arabian Peninsula, the average monthly temperature is between 58℃ and 58℃ for five months a year. Above 30℃. The desert is cooler at night because there are no clouds all night long, the ground radiation is strong, and heat dissipates quickly. The lowest temperature at night is generally between 7°C and 12°C, and there are also days with thin frost.
The annual temperature difference is generally around 10℃~20℃, while the daily temperature difference is even larger, between 15℃~30℃. At a meteorological station south of Tripoli in North Africa, on December 25, 1978, the hottest daytime temperature reached 37.2℃, while the lowest temperature at night dropped to -0.6℃. The daily temperature difference reached 37.8℃. "Leather jacket wears gauze at noon" to describe it.
3. Strong evaporation and low relative humidity: The tropical desert climate is often cloudless, windy, sunny, high in temperature, and low in relative humidity, so the evaporation force is very strong. It is possible that evapotranspiration is more than twenty times, or even a hundred times, that of precipitation. The relative humidity in the air is very small, with a relative humidity of about 2% often found in the Egyptian Sahara Desert.
Tropical monsoon climate
Tropical monsoon climate is only found in southern Asia. There is no tropical monsoon climate in the Southern Hemisphere.
Features: high temperatures all year round, divided into two seasons: dry and rainy, and rainy season.
Cause: The summer monsoon is formed by the seasonal movement of pressure belts and wind belts - the southeast trade winds in the southern hemisphere cross the equator and enter the northern hemisphere, and are deflected to the right under the action of the geostrophic deflection force to become the southwest monsoon. Therefore, the tropical monsoon climate is alternately controlled by the southwest monsoon and northeast trade winds.
In winter, it is mainly caused by the thermal difference between sea and land.
The average temperature in the coldest month of tropical monsoon climate is >15℃. The annual precipitation is between 1500~2000mm. The seasonal distribution is summer rain type.
[Edit this paragraph] Subtropical climate type
Subtropical Mediterranean climate
A climate type in the subtropical and temperate zones. It is named after the most typical Mediterranean coastal area. The most typical reason why the Mediterranean climate is distributed along the Mediterranean coast is that the Mediterranean climate is formed by the alternating control of the westerly belt and the subtropical high pressure belt. In the Mediterranean area, the summer is controlled by the subtropical high pressure belt. The water temperature in the Mediterranean is lower than that of the land, resulting in the formation of high pressure. , increasing the influence of the subtropical high pressure zone, and the water temperature in the Mediterranean is relatively high in winter, forming low pressure, attracting westerly winds, and greatly strengthening the power of westerly winds. Distributed on the west coast of the continent between 30 and 40° south and north latitudes. It is also widely distributed and is the only climate type that is found on all continents in the world except Antarctica.
Climate characteristics:
Summers are hot and dry, with high temperatures and little rain, and winters are mild and humid. The temperature is 5-10℃ in winter and 21-27℃ in summer. The annual precipitation is about 350 to 900 mm, concentrated in winter. The precipitation in the summer half of the year only accounts for 20 to 40% of the annual precipitation. The maximum monthly precipitation is more than three times the minimum monthly precipitation.
Cause:
In summer, under the control of subtropical high pressure, the air flow sinks, resulting in drought and little rain. In winter, the subtropical high pressure moves to low latitudes. The westerly cyclone activity in this climate zone is frequent and precipitation is abundant. At the same time, because the westerly wind blows from the warmer ocean in winter (the thermal properties of sea and land are different), the climate is mild and humid.
Subtropical monsoon and humid monsoon climate
The humid subtropical monsoon climate is distributed on the east coast of the continent between 25° and 35° north and south latitude. It is a combination of tropical ocean air mass and polar continent air mass. A zone of alternate control and mutual competition. The average temperature in January is generally above 0℃, and the average temperature in July is generally around 25℃. The wind direction changes significantly in winter and summer. The annual precipitation is generally above 1000 mm, mainly concentrated in summer. This type of climate is called subtropical monsoon climate in East Asia, and other areas are called subtropical monsoon humid climate due to high precipitation.
Subtropical grassland and desert climate
Subtropical grassland and desert climate are mainly distributed in the south and north, in the western and inland areas of the continent between 25° and 35° latitude. Their basic characteristics are the same as those in the tropics. The climate of the desert is similar, with drought and little rainfall throughout the year, and high temperatures and hot temperatures in the summer. However, due to its slightly higher latitude, the temperature in the winter is lower than that of the tropical desert climate.
[Edit this paragraph] Temperate climate type
Temperate monsoon climate
Temperate monsoon climate occurs on the east coast of the Eurasian continent around 35° to 55° north latitude, including North my country and Northeast China, most of North Korea, northern Japan, and part of the Russian Far East. In winter, affected by northerly winds from high latitudes inland, polar continental air masses prevail here, which is cold and dry; in summer, affected by polar oceanic air masses or modified tropical oceanic air masses, easterly and southeasterly winds prevail, making it warm, hot and rainy, with rain and heat in the same season. The annual precipitation is about 1,000 mm, about two-thirds concentrated in summer (summer is hot and rainy, winter is cold and dry). There are four distinct seasons throughout the year and the weather is changeable. As the latitude increases, the temperature range in winter and summer increases correspondingly, while the precipitation gradually decreases.
Temperate continental climate
Mainly distributed in the Eurasian continent and the inland areas of North America and southern South America at 40° to 60° north latitude. Because it is far away from the ocean, the humid climate is difficult to reach. Therefore, it is dry and rainless, and the climate is extremely continental. The annual and monthly temperature ranges are the highest among all climate types. Moreover, the closer to the center of the continent, the drier it becomes, the greater the annual and daily temperature ranges, and the vegetation also transitions from forests to grasslands and deserts.
The temperate continental climate is located in the interior and the east coast of the continent between 40° and 60--65° north latitude.
In winter, under the control of continental climate, the average temperature in the coldest month is below 0℃ in the south and close to -40℃ in the north. The average temperature in the hottest month is 26-27℃ in the south and close to 20℃ in the north. The growing season lasts about 200 days in the south and only 50-70 days in the north. Those belonging to this climate zone include: Northeast China, most of Siberia, most of Alaska and Canada, and around the Great Lakes of the United States.
The generalized temperate continental climate includes temperate desert climate, temperate steppe climate and subarctic coniferous forest climate. The narrow concept excludes the moist latter. Winter is severely cold, controlled by high pressure, with the lowest temperature reaching -73°C; in summer, the average temperature in July in the south reaches 26-27°C, with the highest temperature reaching 33°C, and in the north it is close to 20°C. The maximum annual temperature range reaches 62.3℃. Controlled by continental air masses all year round, precipitation increases from south to north (from west to east in North America). The annual precipitation ranges from less than 200mm to about 400mm, reaching 300~600mm in the north. The natural vegetation transitions from temperate desert and temperate grassland to subarctic coniferous forest from south to north.
Temperate maritime climate
It is located on the west coast of the continent, in the area of 40° to 60° south and north latitudes. It is in the westerly belt all year round and is deeply influenced by marine air masses. There are warm currents passing along the coast. There is no severe cold in winter and no scorching heat in summer. The average temperature in the coldest month is above 0℃ and the hottest month is below 22℃. The temperature varies from year to year. All small. There is precipitation throughout the year, more in autumn and winter. The annual precipitation is more than 1,000 mm, and it can reach more than 2,000 to 3,000 mm on the windward slopes of mountains. This type of climate is most typical in Western Europe and has the largest distribution area. It is also found in corresponding latitude zones on the west coast of the American continent and in places such as Tasmania and New Zealand in Oceania.
[Edit this paragraph] Frigid climate type
Frigid tundra climate
Distributed on the northern edge of North America and Eurasia (with the hottest month in the south The 10°C isotherm is connected to the subarctic continental climate), part of the coast of Greenland and several islands in the Arctic Ocean; in the southern hemisphere, it is distributed in the Malvinas Islands, South Shetland Islands and South Orkney Islands. . Its characteristics are: winter all year round, with average monthly temperatures between 0° and 10°C for only 1 to 4 months of the year, and the winter is extremely cold and long; the annual precipitation is about 200 to 300 mm, mainly snow; the ground There is a permafrost layer and only low plants such as lichens and mosses.
Cold zone ice sheet climate
Distributed in the polar regions and nearby areas, including Greenland, several islands in the Arctic Ocean and the ice sheet plateaus of the Antarctic continent. This is the birthplace of the icy ocean air mass and the Antarctic air mass. It is in a state of perpetual night throughout the winter. Although there is perpetual daylight in the summer half of the year, the sunlight is oblique and the heat received is weak. Therefore, the climate is severely cold all year round, and the temperature is below 0°C every month; Antarctica The continent's annual average temperature is -25°C, making it the coldest continent in the world. In 1967, Norwegians measured the absolute lowest temperature of -94.5°C, which can be called the world's "cold pole." The ground is mostly covered with thick ice and snow, and there are severe storms, making it difficult for plants to grow.
[Edit this paragraph]Alpine plateau climate
Alpine plateau climate is distributed in the alpine plateau areas of all continents, mainly the Qinghai-Tibet Plateau and its surrounding mountains (Karakoram Mountains, Himalayas , Hengduan Mountains, etc.), the Pamir Plateau and its surrounding areas and the European Alps, the Andes of South America, the Kilimanjaro region of East Africa, etc. The temperature decreases with increasing altitude, with significant vertical changes. From bottom to top, there are tropical, subtropical, temperate, subarctic and permanent snow zones, reflecting a complete spectrum of climate zones. Characteristics of global climate types.
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Mediterranean climate - hot and dry summers, mild and rainy winters
Temperate maritime climate - mild and rainy all year round
Tropical monsoon climate - hot and rainy summers, hot and dry winters , divided into two seasons: rainy and dry seasons
Subtropical monsoon climate - hot and rainy summers, mild and dry winters
Temperate monsoon climate - hot and rainy summers, cold and dry winters
Temperate continental Climate - mild and less rainy in summer, cold and dry in winter
Polar climate - low temperature all year round and little precipitation
Mountain climate - as the altitude increases, the temperature decreases and precipitation changes, and it is rainy on the windward slopes , a brief introduction to the characteristics of various climate types on leeward slopes with little rainfall
Just look at my blog to find out! :hi.baidu./gmllqq/blog/item/867883ec9635a4d42e2e212b.
Climate types and characteristics
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Take a look at the climate type of Guali Town in Xiaoshan District in detail. The characteristics of this climate type are
Subtropical monsoon climate
Characteristics: warm in winter and hot in summer. , four distinct seasons, abundant precipitation, and relatively even seasonal distribution. Characteristics of each climate type and its causes
Characteristics, causes and distribution
Tropical rainforest climate - high temperature and rainy year-round
p>
Affected by the equatorial low pressure belt all year round
Near the equator, between 10 degrees north and south latitude
Tropical grassland climate - divided into dry and wet seasons
It is controlled alternately by the equatorial low pressure belt and the subtropical high pressure
10-20 degrees north and south latitude, west coast of the continent
Tropical desert climate - high temperature and dryness all year round
Perennially affected by subtropical High impact
20-30 degrees north and south latitude, west coast of the continent
Mediterranean climate - hot and dry summers, mild and rainy winters
Alternately affected by westerlies and subtropical high pressures Control
30-40 degrees north and south latitude, west coast of the continent
Temperate maritime climate - mild and rainy all year round
Perennially affected by the westerly belt (warm current warming) Humidification)
40-60 degrees north and south latitude, west coast of the mainland
Tropical monsoon climate - high temperature and rain in summer, high temperature and little rain in winter, divided into two seasons: rain and drought
Differences in thermal properties between land and sea, (South subtropical monsoon, caused by the seasonal movement of pressure belts and wind belts)
15-25 degrees north and south latitude, east coast of the continent
Subtropical monsoon climate- Summers are hot and rainy, winters are mild and less rainy
Differences in thermal properties between land and sea
North and south latitudes 25-35 degrees, east coast of the continent
Temperate monsoon climate - summers are hot and rainy, winters are hot and rainy Cold and dry
Differences in thermal properties between sea and land (monsoon in southwest my country, plus the influence of terrain)
35-55 degrees north and south latitude, east coast of the continent
Temperate zone Continental climate - mild summers with little rain, cold and dry winters
Temperate continental interior, far away from the ocean
Polar climate - low temperatures throughout the year, little precipitation
Divided into tundra zones and ice belts. The tundra zone is mainly along the Arctic Ocean; the ice sheet zone is on the Antarctic continent and Greenland
Mountain climate - as the altitude increases, the temperature decreases, and the precipitation changes. The climate types and characteristics of Antarctica
< p> Rongan County belongs to the mid-subtropical monsoon climate zone. The solar radiation is strong, the climate is warm, the rainfall is abundant, the winter is short and the summer is long, the rain and heat are in the same season, and the climate resources are rich. However, disasters such as low temperature and cold damage, drought, floods, strong winds, and hail also occur in regional areas from time to time. The four seasons are divided according to temperature. The spring in the county is from March 4 to May 15 every year, with an average temperature between 10 and 20°C, counting 73 days; the summer is from May 16 to October 3 every year, with an average temperature of Above 22°C, 141 days are counted; autumn is from October 4 to December 11 each year, and the average temperature is between 10 and 22°C, which is counted as 69 days; winter is from December 12 to March 3 each year, 83 days (84 days in a runnian year), the average temperature is below 10℃. The dryness degree in all parts of the county is below 0.8, with Daliang and Tantou being 0.75 and 0.71 respectively, indicating a humid climate. The remaining townships and towns are all below 0.6, indicating a humid climate. Rongan County is located on the south side of Lingnan. It is the transition zone from the northern Guangxi mountains extending from the Yunnan-Guizhou Plateau to the karst peaks, forest peaks, valleys and Liuzhou platform in central Guangxi. The terrain is complex and forms different regional climates. According to the agricultural climate zoning in the early 1980s, the county is divided into four climate zones.Zhejiang’s climate types and characteristics
Zhejiang has a subtropical monsoon climate with significant monsoons, four distinct seasons, moderate annual temperatures, more sunlight, abundant rainfall, humid air, synchronous seasonal changes in rain and heat, and diverse climate resource configurations. , there are many meteorological disasters.