Briefly describe the climate types in Asia.

There are nine kinds: subtropical and tropical desert climate, tropical monsoon climate, subtropical monsoon climate, temperate monsoon climate, temperate continental climate, cold zone climate, plateau mountain climate, tropical rainforest climate and Mediterranean climate. Among them, the temperate continental climate is the most widely distributed, and the monsoon climate is remarkable.

Attached:

Climate type-distribution-characteristics-vegetation

tropical zone

tropical rainforest climate

On both sides of the equator

It is hot and rainy all year round.

Dense tropical rain forest

Tropical savanna climate

The north and south sides of the tropical rain forest climate

High temperature throughout the year, divided into dry season and rainy season.

tropical grassland

Tropical monsoon climate

South Asia and Southeast Asia

High temperature throughout the year, divided into dry season and rainy season.

Tropical monsoon forest

tropical desert climate

West coast and inland areas near the Tropic of Cancer.

It is hot and dry all year round.

tropical desert

-

temperate zone

Temperate and subtropical monsoon climate

East Asia

The four seasons are distinct and the monsoon is remarkable. The summer monsoon comes from the low latitude ocean, which is hot and rainy; The winter wind comes from the high latitude mainland, which is cold and dry.

Subtropical evergreen and temperate deciduous broad-leaved forest

mediterranean climate

West coast of mid-low latitude continent

Summer is hot and dry, winter is mild and rainy.

Subtropical evergreen broad-leaved forest

Temperate continental climate

Mid-latitude continental interior

Leng Xia is hot in winter, with large temperature difference, less precipitation and concentrated in summer.

Grassland, desert

Temperate maritime climate

West coast of mid-latitude continent

Affected by the warm and humid air flow from the ocean all year round, it is mild and rainy, and the annual changes of temperature and precipitation are small.

Temperate deciduous broad-leaved forest

Coniferous forest climate in sub-frigid zone

Middle and high latitudes near the Arctic Circle.

Winter is cold and summer is mild.

Subhard coniferous forest

-

Alpine cold zone

ice-cap climate

Antarctic continent, an island in the Arctic Ocean

Cold all year round

Snow and ice cover

Ice sheet climate

The northern edge of Asia, Europe and North America.

There is no summer in the long winter

Moss, lichen

mountain climate

Alpine plateau area

Annual low temperature

Ice and snow, cold desert

References:

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Regional differences of world climate and natural landscape

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It is generally believed that the climate formation in a certain place is closely related to five factors. These factors change slightly in a short time, making the climate more stable; For different regions, due to different latitudes, different areas receive different solar radiation energy, different land and sea influences and different atmospheric circulation system configurations, so the climate in different regions has different characteristics. Therefore, to explain the formation of climate, it is necessary to analyze the role of various forming factors and comprehensively consider the influence of each factor on a certain climate.

References:

/GB/earth/weather/system/sys 003 _ 00 . html

China Science Expo-Earth Story > Atmospheric Science Museum > Climate System > Climate Formation.

The role of radiation

The zonal distribution characteristics of astronomical radiation make corresponding zonal climate zones appear on the earth, such as equatorial zone, tropical zone, subtropical zone, temperate zone and cold zone, which are collectively called astronomical climate zones. This is an ideal climate zone. The actual climate is much more complicated, but it forms the basic outline of the global climate.

/GB/earth/weather/system/sys 003 _ 0 1 . html

The role of atmospheric circulation

Atmospheric circulation plays an important role in climate formation. It not only affects the zonality of climate through the zonal distribution of circulation, but also expands the influence range of land, ocean and terrain through the transport of heat and moisture, and destroys the zonality of climate. When the circulation situation tends to the long-term average situation, the climate is normal; When the circulation situation is abnormal in individual years or seasons, it will directly affect the weather and climate of that period and make it abnormal.

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Influence of land and ocean distribution on climate

The ocean accounts for 7 1% of the total area of the earth, and the land only accounts for 29%, so the difference between land and sea is the biggest and most basic difference of the underlying surface. Due to the different physical properties, under the same radiation, the warming and cooling of the ocean and the mainland are completely different. In winter, the temperature of the mainland is lower than that of the ocean, and in summer, the temperature of the mainland is higher than that of the ocean.

Seen from the upper troposphere at sea level, the land temperature was lower than the ocean in May 438+10. July is the opposite. The difference between them in July was greater than1; The lower level is bigger than the upper level. Last year, the land annual range was worse than the ocean.

Land and sea also have obvious influence on air pressure and wind force. The pressure distribution varies with the temperature distribution. In summer, the mainland is the heat source and the ocean is the cold source, so the air pressure on the land is low and the air pressure on the sea is high, and the wind blows from the ocean to the mainland; In winter, the ocean is the heat source and the mainland is the cold source. Sea water pressure is low, land pressure is high, and wind blows from land to sea. In addition, land and sea have great influence on humidity, cloud cover, fog and precipitation.

Land and sea have a great influence on climate, forming a completely different continental climate and maritime climate on the earth.

The difference between maritime climate and continental climate,

-In terms of temperature, the continental climate is characterized by rapid change and large amplitude, so the daily range and annual range value of the continental climate are large, while the maritime climate is the opposite. The highest temperature in continental climate appears in July, and the lowest temperature appears in 65438+ 10.

Generally, the highest temperature in maritime climate appears in August, and the lowest temperature appears in February, and the temperature change lags behind that in Chinese mainland. At the same latitude, the temperature in spring and summer,

The land is higher and the sea is lower; On the contrary, the land temperature is lower and the sea temperature is higher in winter and autumn. Therefore, the continental climate has the characteristics that the temperature in spring is higher than that in autumn, and the maritime climate has the characteristics that the temperature in autumn is higher than that in spring.

-In terms of humidity and precipitation, the maritime climate is characterized by high relative humidity, small annual variation of relative humidity, large cloud cover and precipitation, small annual variation of precipitation and more precipitation in autumn and winter. Continental climate is characterized by low relative humidity, large annual variation of relative humidity, less cloud cover, more sunny days, less precipitation, large annual variation of precipitation and more precipitation in summer.

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Topography and climate

Terrain ups and downs not only make their own climate differences significant, but also towering mountains are often obstacles to the flow and operation of low-level air, which can block the cold air in the north and the warm air in the south (such as blocking the cold wave, making the front belt stagnate) and make a lot of water loss in the airflow.

(1) temperature effect

(2) Impact on precipitation

(3) Mountain stereoscopic climate

/GB/earth/weather/system/sys 003 _ 04 . html

Ocean currents and climate

The nature of the ocean underlying surface is uneven, and the difference is mainly manifested in the cold and warm currents.

Ocean current is an important driving force of heat transfer on the earth.

The influence of ocean currents on climate is mainly indirectly produced through air mass activities. Because ocean current is the underlying surface of the air mass above it, it can denature the lower part of the air mass, and when the air mass moves, it will bring these characteristics to the passing area, thus changing the climate. Generally speaking, the climate along the coast where the warm current passes is warmer than that near the same latitude; Along the coast where cold ocean currents pass, the climate is colder than around the same latitude.

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Influence of snow and ice cover on climate

Snow and ice cover is one of the components of the climate system. Because of their radiation and other thermal properties, sea ice, continental ice sheet, alpine glacier and seasonal snow are very different from the ocean and the land without ice and snow cover. They form a special underlying surface, which not only affects the climate in the region, but also has a great impact on the atmospheric circulation, temperature and precipitation in another continent and hemisphere. Snow and ice cover is an important factor in climate formation.

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..... resources

/GB/ Earth/Weather/System/Index.html

China Science Expo-Earth Story > Atmospheric Science Museum > Weather System

I copied a little from other places, hehe, but it's not a secret.

Anyway, I hope I can help you.

Remember to add my point. )