Why is the asian monsoon climate the most striking
Reason: mainly affected by land and sea distribution。
It is located between the world's largest continent, asia-europe, and the largest oceanic pacific, due in particular to differences in the nature of thermal power of land and sea。
Performance: east asia experienced south-east monsoons in summer, north-west monsoons in winter and hot seasons, and south-west monsoons in south asia in summer and north-east monsoons in winter, with clear dry and wet seasons。
Why is there a tropical, temperate monsoon climate in asia and not in other continents
Asia alone has a tropical monsoon climate: the winter in south asia is affected by variations in the nature of the heat from sea to land, blowing the north-east monsoon, during the summer, owing to seasonal shifts in the air-pressure and wind belts, shifting south-east to south-west monsoons after the equatorial period, and bringing precipitation from the indian ocean to south asia. In other continents, this latitude is located in the upper-wind zone of the intra-wind wind belt, where the surface area is small, thus preventing the formation of tropical monsoons。
Asia alone has a temperate monsoon climate: asia is located between the largest continents and the largest oceans, with significant variations in the nature of surface and surface heat, with summer winds extending to higher latitudes, while other continents are less affected by summer winds because of smaller variations in the nature of surface and surface heat. Only asia has a temperate monsoon climate。
3. How does monsoon weather change around the world
Subtropical and temperate monsoon climates in the northern hemisphere: south-east in summer and north-west in winter; south-west in summer and north-east in winter. The monsoon climate in the southern hemisphere: the summer winds to the north and the winter to the south。
4. Causes of the tar desert
The formation of the tar desert is related to the summer wind:
(1) the tar desert forms thermal low pressure during the summer, but is controlled by sub-highs at high altitude, and sub-sinks are prevalent, creating a high-low-pressure stacking, which prevents the low-pressure flow from rising further and becomes cloudy。
(2) the south-west air current is dryer than it is in the arab world and africa。
5. Why does the sahara trans-african ocean extend to the seaside
Years have been affected by sub-highs and bands, as well as by tropical continental air groups. The west side is affected by cold currents in canary, with cooling and dampness, and the east side with the red sea, but because of the small body of water, the climate is dry and precipitation is scarce。
6. Causes of the sahara desert
(1) the atlantic coast is affected by the canary cold, affecting the coast from north to south and stabilizing the atmosphere。
(2) the mediterranean sea is affected by relative pressure, which is relatively low in the winter, where the pressure is irradiated, while tropical continental air groups affect the mediterranean sea, which is relatively high in the summer, with strong downpours, sunk the mediterranean coast and deepened the drying of the sahara desert climate。
(3) the red sea is a narrow water column, the north-east is an arab desert zone, the north-east is a dry gas stream, situated in a sub-tropical sea zone, with high temperatures, high salt and stable atmosphere。
(4) the sub-high of the south can be up to 18o n。
7. Causes of the namib desert
The air is dry as a result of high sub-tropical pressure and the south-east of the country, and there is a cold flow of benguela along the coast, which reduces temperature and humidity。
8. Causes of the atacama desert and its northward extension to the equator
As cold flows pass through the coast, making the near surface a cooling source, the atmosphere is inversely warm off the coast, resulting in the inability of the atmosphere to rise continuously and form a tropical coastal mist desert。
9. Causes of the takrama desert
The fact that the region is landlocked, not affected by the summer wind of monsoon circulation on the eastern coast of the continent, and not by the west-west wind of the three rings of the west bank of the continent, results in scarce precipitation, creating a temperate inland desert zone。
10. Reasons why the namib desert did not extend to the east coast
(1) dry thermal currents shall not affect the east coast, which is blocked by the topography of the south african plateau。
(2) there is a warm flow along the coast of the east coast, which brings abundant water vapour。
11. What is the cause of tropical desert climate on both sides of the red sea
Both sides are located near the northern line of return and are constantly controlled by the subtropical high-pressure belt and the north-east band, evaporating and hot and dry. And the narrow surface of the red sea does not bring precipitation to the two shores。
12. Causes of the california desert
It was influenced by sub-highs and by the cold flow of california。
13. Is western central australia the cause of desert climate
It has been affected by sub-highs, wind belts and cold waves in western australia。
14. What are the causes of the climate in the congo basin rainforest and why is it not extended to the east coast
Between 10o north and south, the equatorial low-pressure belt is constantly affected by rising air currents and high temperatures and rainfall throughout the year。
(1) the east is the east african plateau with a high terrain, a flow from the gulf of guinea, and the south-east indian ocean has precipitation along the coast but has difficulty accessing the east african plateau。
(2) south-west air currents are shallow and even thinner when they enter the east african plateau, where rainfall is low and the east african plateau is tropical savannah weather。
(3) the movement of air-pressure wind belts, which are at 18o n in the south summer of the north and south of the south winter, with short passage through the highlands of east africa and low precipitation。
15. The cause of the creation of the world's largest rainforest climate zone in the amazon plain
The amazon plain is vast and flat, located near the equator in the north of south america, and is constantly controlled by low equatorial pressure and the winds of faith, with high air-to-flow. Its north, west and south are plateaus, mountains, open east to the atlantic ocean, and warm coastal flows, which gather inland from the north-east, south-east sea, and are driven up by western mountains, with abundant precipitation throughout the year. As a result, the amazon plain has become the world's largest tropical rainforest weather zone。
16. What are the causes of climate differences between the eastern and western shores of madagascar
The eastern coast of madagascar is on the south-eastern wind-winding slope, and madagascar is warm enough to receive more rainfall. The west bank, on the other hand, is in the position of a windy slope, with the main wind blowing off the coast, resulting in less precipitation。
17. Causes of the rainforest climate in north-eastern australia
In the summer, controlled by the equatorial low-pressure belts, rising air currents are prevalent and precipitation is high; in the winter, north-east is affected by the south-east wind, which blows from the sea, is more abundant in water, and there is a warm flow along the coast of east australia, increasing its water vapour content, so that the eastern part of australia is tropical rainforest weather。
18. Causes of climate change in the rainforest south-east of the brazilian plateau
Constantly influenced by the heat flow from brazil, the temperature increases and the humidity increases; the south-east wind-receiving slope, with abundant rainfall; and the low latitude and high temperature。
19. Why is the desert in the arabian peninsula, which is a tropical monsoon climate, compared to the indian peninsula at the same latitude
The three sides of the arabian peninsula are surrounded by land, controlled by the north-east wind belt and the sub-tropical high-pressure belt, with a tropical continental air mass, with low water and gas content from land to the arabian peninsula。
The three sides of the indian peninsula are sea, and in the summer, the air-pressure wind is moved northwards, the south-east is transformed from an equatorial to south-west wind, which blows from the northern indian ocean to the indian peninsula, bringing abundant precipitation and a rainy season
In winter, the air-pressure wind is moving southwards, causing the indian peninsula to become more affected by the north-east wind wind in the north-east monsoon, when the asian continent is experiencing cold and high pressure, and air flows are dispersed around it, affecting the indian peninsula, reducing its precipitation to a dry season。
The equatorial region of eastern africa is not a tropical rainforest climate but rather a tropical savannah climate
East africa is an east african plateau with a high terrain, which makes it difficult for warm and wet water vapours along the coast to reach the east african plateau, creating a tropical savannah climate。
21. The northern part of the gulf of guinea in africa is the cause of tropical rainforest climate
Increased temperature and humidity as a result of the warm flow of guinea。
22. Why is the mediterranean climate the most widely distributed along the mediterranean coast and its small size on other continents
The mediterranean coastal area coincides with the opening to the west of the mediterranean coast, which is affected by the western wind belt during the winter when water vapour enters the mediterranean and affects the coastal areas. Others are affected by the terrain and are relatively small。
What are the reasons for the wide north-south temperature difference and the large north-south-south-west variability of precipitation in japan
(1) japan has a long and complex terrain and different latitudes between north and south, leading to wide variations in temperature between north and south。
(2) the difference between north-west and south-east of precipitation is due to the oceanic nature of japan's monsoon climate. Japan has a complex terrain, dominated by hills and hills, and mountains are situated in the same direction as the islands, extending from north to south. In the summer, the south-east is located in the south-east monsoon slopes, with more precipitation, and the north-west is on the side of the back wind, with less precipitation; in winter, the north-west is on the north-west wind slope, which, following the passage of the japanese sea, increases water vapour levels, resulting in more snowfall in the north-west, while the south-east is on the side of the back wind, with less precipitation. In general, however, north-west precipitation in japan is smaller than south-east。
24. Why is the north-south climate so different on the korean peninsula
The north and south of the korean peninsula have a much larger latitude, a lower latitude in the south and a warm current from japan, a subtropical monsoon climate, a far north from the sea and a much higher latitude, and a much higher winter wind effect, resulting in lower winter temperatures and a temperate monsoon climate。
25. The differences and causes of winter and summer winds in java
In the summer, affected by the south-east wind, the south-east monsoon was blown, and in the winter north-east, the wind passed the equator and turned to the north-west monsoon, affecting java. Reasons: pressure bands, movement of wind belts and influence of geo-diversion。
