From June until September, summer monsoon rains occur in South Asian countries such as Vietnam, Thailand, Cambodia, Bangladesh, Laos, India, and Pakistan. From December until February, the monsoon rains move south of the equator towards Australia while South Asia experiences dry monsoon conditions.
However, monsoons are not the same throughout the tropics, because the specific locations of continents and oceans influence the regional patterns of winds and rain. Classic conditions for strong monsoons are found where the Indian Ocean and the Pacific Ocean meet.
The most prolific districts on the earth square measure the tropical and therefore the sub-tropical locales. The Ganga-Brahmaputra Basin is the biggest sub-tropical space in Asia and the variety of people living here is quite elsewhere in the world.
Strong swings between wet summers and dry winters are found in those places as the ITCZ moves back and forth across the equator. The South Asian monsoon, which includes the Indian monsoon, is especially strong because the Himalayas and other mountains block dry air in the north from getting to the humid monsoon region.
Across the Asian continent, typical monsoon climates can be found in the central and southern Indian subcontinent and Indochina, connecting to the weak monsoon regions in southwestern, southern, and eastern China.
A tropical wet climate is found in coastal parts of Myanmar, Thailand, Vietnam, and Oceania, and in most of Malaysia, Indonesia, and the Philippines. Temperatures are high.
Mainly at risk are large delta regions of Bangladesh, Myanmar, Vietnam and Thailand, and the low-lying areas of Indonesia, Malaysia and the Philippines.
Monsoon Asia refers to the portion of the Asian continent where a significant seasonal shift of wind patterns occurs throughout the entire area. The region includes the Indian subcontinent, Southeast Asia, and China.
Eastern Asia is home to three main climates. In the north, you'll find a mix of semi-arid (west) and humid continental climates (east). The south is largely humid subtropical. As you head into the mountains in the west, things get dryer.
Much of Southeast Asia is within the tropical climatic zone with temperatures above 25 deg C throughout the year. The region is strongly influenced by the Asian monsoons, which bring significant amount of rainfall to parts of Southeast Asia.
The tropical climate zone in East Asia is fairly small. It includes a small strip of land along China's southeastern coast, the island of Hainan, and the southern tip of Taiwan. These areas have high temperatures, heavy rainfall, and high humidity every month of the year.
East Asia, especially Chinese civilization, is regarded as one of the earliest cradles of civilization. Other ancient civilizations in East Asia that still exist as independent countries in the present day include the Japanese, Korean and Mongolian civilizations.
In winter continental tropical air prevails in tropical Asia; in summer it is replaced by equatorial ocean air.
Answer: As winter ends, warm, moist air from the southwest Indian Ocean blows toward countries like India, Sri Lanka, Bangladesh, and Myanmar. The summer monsoon brings a humid climate and torrential rainfall to these areas. India and Southeast Asia depend on the summer monsoon.
The major controlling factor over a tropical monsoon climate is its relationship to the monsoon circulation. The monsoon is a seasonal change in wind direction. In Asia, during the summer (or high-sun season) there is an onshore flow of air (air moving from ocean toward land).
Monsoons cause wet and dry seasons throughout much of the tropics. Monsoons are most often associated with the Indian Ocean. Monsoons always blow from cold to warm regions. The summer monsoon and the winter monsoon determine the climate for most of India and Southeast Asia.
An area of tropical monsoon climate (occasionally known as a tropical monsoon and trade-wind littoral climate) is a type of climate that corresponds to the Köppen climate classification category "Am". Tropical monsoon climates have monthly mean temperatures above 18 °C (64 °F) in every month of the year and a dry season.
During the rainy season, heavy rains can cause disruption to infrastructure and airport emergency services. Thunderstorms can be accompanied by severe downdrafts and heavy rain causing flooding on airport surfaces and the risk of aquaplaning on runways. Strong thunderstorms and high winds are more common with the onset of the monsoon rains.
From December until February, the monsoon rains move south of the equator towards Australia while South Asia experiences dry monsoon conditions. There is even an East Asian monsoon that brings summer rain to China, Japan, and Korea, but it is caused by a different type of wind pattern associated with the jet stream.
However, monsoons are not the same throughout the tropics, because the specific locations of continents and oceans influence the regional patterns of winds and rain. Classic conditions for strong monsoons are found where the Indian Ocean and the Pacific Ocean meet.
The South Asian monsoon, which includes the Indian monsoon, is especially strong because the Himalayas and other mountains block dry air in the north from getting to the humid monsoon region.
From June to August, which are summer months in the Northern Hemisphere, there is more rainfall north of the equator in Costa Rica, Nicaragua, Panama, and western Mexico. From December to February there is more rainfall south of the equator in Brazil.
Asia, India, and Australia. With the world’s strongest monsoons, this region stretches from the South China Sea into the Indian Ocean and includes Asia and the northern end of Australia. From June until September, summer monsoon rains occur in South Asian countries such as Vietnam, Thailand, Cambodia, Bangladesh, Laos, India, and Pakistan.
The Americas. Monsoon winds in the tropical parts of North America, Central America, and South America cause the amount of rainfall to vary with the seasons, even in areas where precipitation is plentiful and rainforests thrive. From June to August, which are summer months in the Northern Hemisphere, there is more rainfall north ...