Traditional Culture Encyclopedia - Weather inquiry - What is the highest temperature of Congo cloth?
What is the highest temperature of Congo cloth?
Origin of tropical rain forests in Congo Basin and Gulf of Guinea: The climate in equatorial region is always hot, humid and rainy within the range of north-south latitude 10. It is 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 Peninsula, the Philippine Islands and Irian Island, and Oceania from Sumatra Island to New Guinea. Several areas are wet all the year round. The hot and humid climate and abundant rainfall there provide excellent environmental conditions for the growth of plants. In these areas, dense forests are evergreen all year round, just like a jade necklace around the earth, which is the basic feature of tropical rain forests. For example, Iquitos is usually higher than 1800 mm, and it reaches 3500 mm in some places. There is no obvious seasonal change here, and the daytime temperature is generally around 30 degrees Celsius. It's about 20 degrees Celsius at night. It is also distributed in Yunnan, Taiwan Province Province, Hainan, parts of Australia and Madagascar. Affected by the above factors, the dominant factors of tropical rain forest are still different. The general trend is mainly influenced by solar radiation in the range of north-south latitude 10 degrees in the equatorial region. The equatorial low pressure zone and trade winds gather near the equator, and the water vapor contained in it is easy to form clouds and cause rainfall. It is summer all the year round. It is usually sunny in the morning, hot before noon, rainy in the afternoon, and the weather is a little cold. However, in the same type of region in the world, the tropical evergreen rainforest in the Amazon Plain is not only the most extensive, but also the most fully developed and typical. This is because the geographical location of the Amazon Plain is crossed by the equator, with Guiana Plateau in the north, Brazil Plateau in the south and Andes in the west, just like a chair. Open arms to accept the abundant warm and humid air currents brought by the northeast and southeast trade winds and the warm currents of the north and south equator, which makes it have modern climatic conditions that are particularly conducive to the development of this type. On the other hand, it is also related to its long history of development and relatively stable natural and geographical conditions during its formation. The Amazon River is the second longest river in the world. It runs through South America from west to east, with a basin area of 6 million square kilometers. It is covered with dense jungle. The mainstream of the Amazon River sometimes overflows, flooding thousands of square kilometers of forest land. It is the river with the largest runoff in the world, and the comprehensive characteristics of its genesis are very obvious. Affected by topography, ocean currents and monsoons, the tropical rain forest climate in Africa is limited to the Congo River basin in Africa and the coastal areas of the Gulf of Guinea. The main reason is that the equator passes through the Congo basin in Central Africa and East Africa. Due to the plateau topography of East Africa, it belongs to the tropical plateau in climate. Under the influence of southwest monsoon and Guinea warm current, moist water vapor will seep into the basin from the estuary, and under the influence of equatorial low pressure, it will converge and rise, with abundant rainfall throughout the year. Therefore, the Congo River, a river flowing through this area, is rich in water, which is very conducive to navigation. The continental characteristics of tropical rainforests are obvious. In Asia, the southwest coast of the Indian Peninsula, the Malay Peninsula and the west coast of the Indian zhina Peninsula, the Philippine Islands, Irian Island and Oceania from Sumatra Island to New Guinea are scattered in the ocean, mainly affected by solar radiation. In addition, the rainforest climate here has outstanding marine characteristics. Although some areas are not between north and south latitudes 10 degrees and are not affected by equatorial depression, the climate of tropical rain forests sometimes presents non-zonal characteristics due to the interaction of atmospheric circulation and ocean currents. For example, the formation of rainforests in Yunnan, Taiwan Province, Hainan and parts of Australia in China, Madagascar and Florida Peninsula in the United States are all closely related to topography and ocean currents. For example, influenced by the South Equatorial Warm Current and the Southeast Trade Wind, the warm and humid airflow climbs along the windward slope in the eastern part of the Madagascar Mountains. Although the Tropic of Capricorn passes through, the southeast coast has a tropical rainforest climate. The central part has a tropical plateau climate and the western part has a tropical grassland climate. The annual average temperature 18-26 degrees, and the annual precipitation decreased from 2000-2000 mm in the east to 750- 1000 mm in the west. Similarly, the formation of tropical rain forest in northeastern Australia is also influenced by topography, warm current in eastern Australia and southeast trade winds. The formation of rainforests in China, Yunnan, Taiwan Province, Hainan and Florida Peninsula is similar to the above characteristics. Even the East African Plateau near the equator mentioned above has formed a tropical grassland climate because of its topography, and the coastal area south of Congo Basin on the west coast has formed a tropical desert climate under the influence of Benguela cold current and South Equatorial Rift. There are tropical deserts on the west coast of South America, which extend the longest from north to south and are closest to the equator. The climate is dry and the temperature is low. In short, through the analysis of the differences in the causes of tropical rain forests, it is helpful for senior three students to understand and master the global climate types by using the knowledge of global atmospheric circulation and ocean currents and the topographic characteristics of various continents. Looking forward to your satisfaction ~
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