What are the climate types in Asia and Europe? 1, tropical desert climate. 2. Subtropical monsoon climate. 3,

Asia: (from south to north) tropical rain forest climate, tropical monsoon climate, alpine climate, subtropical monsoon climate, temperate monsoon climate, temperate continental climate, polar climate, etc.

(1) In East and South Asia, the monsoon climate is remarkable. Indo-China Peninsula and Indian Peninsula mainly belong to tropical monsoon climate. High temperature throughout the year, southwest monsoon prevails in summer, and precipitation is scarce. The southern part of the Malay Peninsula and most parts of the Malay Archipelago are hot and rainy all year round and belong to the tropical rainforest climate.

East China, Korea and Japan belong to temperate monsoon climate and subtropical monsoon climate. Southerly winds prevail in summer, with high temperature and rainy weather, while northerly winds prevail in winter, with cold and dry weather.

(2) The central and western parts of Asia are located inland, which is less affected by the ocean and belongs to the continental climate of arid temperate zone.

(3) In northern Asia, the winter is long and the temperature is very low; Summer is short, but mild. Most of the areas there belong to the sub-frigid coniferous forest climate in temperate continental climate, with the largest coniferous forest belt in the world. Only the northern coast of Siberia and the islands in the Arctic Ocean are extremely cold all year round and have a polar climate.

(4) The Arabian Peninsula in the southwest of Asia and the Indus Plain in the south are hot all the year round, with small precipitation and large evaporation, forming a tropical desert climate. The Mediterranean coastal area is influenced by westerlies in winter and subtropical high in summer, which belongs to the Mediterranean climate, with rainy winter and dry summer.

(5) The Qinghai-Tibet Plateau and some alpine areas in Central Asia are more than 4,000 meters above sea level, with low temperature all year round and many snow-capped glaciers, which belong to alpine climate.

Europe: Mediterranean climate, temperate maritime climate, temperate continental climate, polar climate.

Main climatic zones in Europe:

(a) polar ice climate zone

The ice sheet climate exists only on the islands of the Arctic Ocean. It is controlled by the ice air mass all the year round, and the temperature is very low. In the hottest month, the average temperature is about 0℃, and the annual precipitation is about 200 mm. In the west of Spitsbergen Islands, influenced by the North Atlantic warm current, the climate is slightly mild, and the average temperature in the hottest month can reach about +5℃, and the precipitation can reach 300 mm.

(2) Polar tundra climate zone (polar long cold climate zone)

This area includes Iceland and the northern edge of continental Europe. The temperature here is low all the year round, and the landscape belongs to tundra zone and Forest tundra zone. In winter, the temperature in the west is higher than in the east. The average temperature in Leng Yue in Iceland's coastal area is around 0℃, in Murmansk's coastal area it is around -0.5℃ in June 5438+1October, and in Kanin-Bojola in the east it drops to around -20℃. In summer, the temperature is generally around 10℃, the growth period is very short, only 2-2.5 months, and even there is often frost in summer, so the climatic conditions are very unfavorable to agriculture. There is almost no farming operation here, and animal husbandry (mainly deer industry) is the main agricultural department here.

(3) sub-rigid coniferous forest climate zone (sub-rigid continental climate zone)

This area includes most of Fenos Candea and the northern part of Eastern Europe Plain. The latitude here is high, the winter is long, but it is rarely cold, and the summer is short and cool. The western coast of Scandinavia is controlled by polar ocean air mass all the year round, and the climate is maritime. In winter, the temperature is around 0℃ and there is abundant precipitation. From the east of Scandinavian Mountains to the Urals Mountains, the role of polar continental air mass and ice air mass is enhanced, the climate changes to continental, the winter is cold, and the temperature drops from west to east. In 65438+ 10, the average temperature in Gaffler is -4.4℃, in Petrozavodsk it is -9.9℃, and in Perm it is-15.4℃. Whenever an ice air mass invades, severe cold of -30℃ and -40℃ often occurs. It is usually cool in summer. The average temperature in July is 10- 12℃ in the north and 16- 18℃ in the south. The growth period is not long, usually 3-4 months. The growth temperature (above 10℃) suitable for rye, flax and vegetables in Eastern Europe lasts only 90 days at most, so the agriculture here is also underdeveloped.

The precipitation here is mainly related to cyclones. The annual precipitation in the western coastal areas exceeds 1000 mm, and the annual precipitation in other areas is 500-800 mm. The seasonal distribution of precipitation in the western coastal areas is relatively uniform, with a little more in winter and a little more in summer in the east. Besides cyclone precipitation, convective rain also accounts for a certain proportion.

(4) temperate maritime climate zone

This region includes the British Isles, France and western Central Europe, as well as the southern Scandinavia and the coastal areas of the Bay of Biscay in Iberia. The atmospheric pressure here is high in the south and low in the north all the year round, with a westerly wind, which is deeply influenced by the Atlantic air mass. Mild winter, cool summer, low annual temperature, more rain and less sunshine are the climate characteristics of this area.

The average temperature in June 65438+ 10 in this area is above 0℃. Rivers generally don't freeze. There is not much snowfall, generally it doesn't snow in the west, and the snow period in the east rarely lasts more than a week. However, when the Mongolian high pressure is very strong and the eastern polar continental air mass invades, it often leads to disastrous low temperature weather. Generally, the temperature is not high in summer The average temperature in July in the British Isles is 12- 17℃, and in the mainland it is 15-22℃. The temperature is lower in the north and higher in the south.

Western Europe has frequent cyclone activities and more precipitation. The annual precipitation in the western part of the British Isles is above 1000 mm, and the coastal area in western Scotland can reach above 2000 mm. Other areas are mostly between 600-1000 mm. The seasonal distribution of precipitation is relatively uniform, with more in autumn and winter in the west and more in summer in the east. For example, Dublin accounts for 26% in autumn and winter, and 24% in spring and summer; Cologne accounts for 365,438+0% in summer, 25% in autumn, 23% in winter and 265,438+0% in spring.

(5) temperate continental climate zone

The region includes temperate continental humid climate and temperate continental semi-arid and arid climate. Generally speaking, Eastern Europe and Central Europe belong to the former, while Southern Europe and Eastern Europe belong to the latter.

The climate in eastern Central Europe has the nature of transition from maritime to continental. The influence of polar ocean air mass is dominant here all year round, with mild winter and low temperature in summer. The average temperature in 65438+ 10 is generally 0-4℃, which can reach -5℃ in a few areas, and the average temperature in July is generally around 18℃, which can exceed 20℃ in a few areas. However, ice air masses and polar continental air masses often invade, so the weather is very unstable. Precipitation is greatly influenced by topography, which is generally 500-600 mm in plain areas and more in summer.

The climate in eastern Europe is divided into two regions: the north and the south. The mixed forest belt in the middle is in the north, which belongs to the humid continental climate. It is greatly influenced by the polar ocean air mass. There is no severe cold in winter and the temperature will not be too high in summer. The average temperature in 65438+ 10 is between -5℃ and 14℃ in most areas, and the average temperature in July is less than 20℃. The annual precipitation is generally 500-600 mm, which is more in some areas. The southern region is located in the Eurasian high-pressure axis (called "Voyekov high-pressure axis" by the Soviets) and the area south of the high-pressure axis, and the related westerly airflow and cyclone activities are obviously weakened, and the anticyclonic weather is increasing. The annual precipitation is generally 300-500mm, the southeast is below 200mm, and the summer temperature is between 20-25℃. The water balance of the whole southern district is negative, belonging to temperate continental semi-arid and arid climate. In the natural landscape, most areas are grasslands, and the southeast is semi-desert or desert. Southern district is rich in heat resources and fertile land, and it is the main agricultural area. However, due to insufficient precipitation and great changes, droughts often occur.

(6) Mediterranean climate zone

This region includes most of Iberian Peninsula, French Mediterranean coast, Apennine Peninsula, most of Balkan Peninsula and various islands scattered in the Mediterranean. Mild and rainy winter and hot and dry summer are the main characteristics of the climate in this area.

Mediterranean climate is a unique climate type on the west coast of subtropical continent, and its formation is related to the change of air pressure situation in winter and summer and the movement of wind belt. The latitude of the Mediterranean region is just the transition zone of atmospheric circulation; The westerlies are in the north and the trade winds are in the south. In summer, the subtropical high moves northward. Under the control of azores high, the weather in the Mediterranean is sunny and dry. The average temperature in July reaches 24-28℃, and the highest temperature can reach 40℃. In winter, the subtropical high moved south, and azores high retreated to the Atlantic Ocean. The Mediterranean region is affected by the west wind, with frequent cyclone activities, more precipitation and mild climate, with an average temperature of 1 month.

The existence of the Mediterranean itself also plays a great role in the formation of the Mediterranean climate. Due to the large area of the Mediterranean Sea, a low-pressure lake is formed in the Mediterranean Sea in winter, which is conducive to the formation of the Mediterranean front, resulting in a series of cyclones, making the weather in the Mediterranean Sea particularly mild and rainy. At the same time, the higher Mediterranean water temperature also makes the coastal areas more temperate; In summer, on the contrary, the temperature in the Mediterranean is lower than that in continental Europe, and the air pressure is higher, which strengthens azores high and makes the Mediterranean region very hot and dry. In this way, the most typical subtropical climate in the world has been formed in the Mediterranean region, with warm winter, rainy summer and dry heat. Therefore, it is called "Mediterranean climate".

In the mountainous areas with the above climatic zones, the climate is more complicated. Because of the different heights, cutting conditions and slope directions of mountains, the climate changes greatly in a short distance. On higher mountains, the climate changes vertically.