The Beauty of the Tropical Monsoon Climate
The tropical monsoon climate is found in those regions where there is a complete seasonal reversal of winds. It is mainly found beyond the equatorial region between 10° and 25° North and South of the Equator. On-shore summer winds blowing from over tropical warm oceans generate the abundant precipitation, while the off-shore winds from over land make the weather dry during winter. The most clearly defined monsoon climates are located in the coastal areas of the eastern and southern Asia. For example, India, Burma, Bangladesh, Indochina, Southern China and the Philippines experience a tropical monsoon climate. Surface relief, direction of the coast line and the extension of the monsoon into middle-latitudes cause a number of sub-types of the monsoon climate found over this most widespread continent.
Rains are abundant and intense in tropical monsoon areas. But there is a distinct dry season, though very short. However, the amount of precipitation during the rainy season is so heavy that it more than gives back the absence of rainfall for a few months. Soils retain moisture to support the plant cover. In the tropical monsoon climate summer is generally the rainy season. During the high-sun period the on-shore winds bring a lot of moisture from over the tropical warm oceans to the land. Wherever these moisture-laden winds are forced to rise, abundant precipitation results. However, the coastal regions, if backed by highlands, receive the maximum amount of precipitation. It is important that the leeward sides of the coastal ranges suffer from the rain shadow effects. During the winter monsoon period, January and February are the driest months in South-east Asia. The distribution of rainfall in the subcontinent is more uneven than elsewhere. The rainfall decreases from east to west and from north to south in so much so that the western and north-western regions have almost semi-arid climate.
The monsoon circulation in South-east Asia is characteristically governed
Rains are abundant and intense in tropical monsoon areas. But there is a distinct dry season, though very short. However, the amount of precipitation during the rainy season is so heavy that it more than gives back the absence of rainfall for a few months. Soils retain moisture to support the plant cover. In the tropical monsoon climate summer is generally the rainy season. During the high-sun period the on-shore winds bring a lot of moisture from over the tropical warm oceans to the land. Wherever these moisture-laden winds are forced to rise, abundant precipitation results. However, the coastal regions, if backed by highlands, receive the maximum amount of precipitation. It is important that the leeward sides of the coastal ranges suffer from the rain shadow effects. During the winter monsoon period, January and February are the driest months in South-east Asia. The distribution of rainfall in the subcontinent is more uneven than elsewhere. The rainfall decreases from east to west and from north to south in so much so that the western and north-western regions have almost semi-arid climate.
The monsoon circulation in South-east Asia is characteristically governed