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The Monsoon of South Asia is among several geographically distributed global monsoons. It affects the Indian subcontinent , where it is one of the oldest and most anticipated weather phenomena and an economically important pattern every year from June through September, but it is only partly understood and notoriously difficult to predict.
Seasonal (mixed) tropical forests can be found in many parts of the tropical zone, with examples found in: In the Asia-Pacific region: seasonal forests predominate across large areas of the Eastern Java, Wallacea, Indian subcontinent and Indochina. Eastern Java monsoon forests; Wallacea Forest; Brahmaputra Valley semi-evergreen forests
An area of tropical monsoon climate (occasionally known as a sub-equatorial, tropical wet climate or a tropical monsoon and trade-wind littoral climate) is a tropical climate subtype that corresponds to the Köppen climate classification category Am. Tropical monsoon climates have monthly mean temperatures above 18 °C (64 °F) in every month ...
The monsoon rain forest ecoregion encompasses the interior mountain range, surrounded by the coastal plains. (The coastal plains fall in an entirely different ecoregion - the South China-Vietnam subtropical evergreen forests ecoregion). The highest point in the Hainan mountains is Wuzhi Mountain at 1,840 metres (6,040 ft). There is a small ...
Tropical seasonal forests, also known as moist deciduous, monsoon or semi-evergreen (mixed) seasonal forests, have a monsoon or wet savannah climates (as in the Köppen climate classification): receiving high overall rainfall with a warm summer wet season and (often) a cooler winter dry season. Some trees in these forests drop some or all of ...
The Andaman and Nicobar islands have tropical evergreen forests and tropical semi-evergreen forests as well as tropical monsoon forests. [4] The dominant species of Keruing wood is Dipterocarpus grandiflorus in hilly areas, while Dipterocarpus kerrii is dominant on some islands in the southern parts of the archipelago .
Forest coverage is about 70% tropical dry monsoon forests, 15% tropical moist monsoon forests and 5% tropical lower montane forests. By the dawn of the 19th century, Sri Lanka's forest cover was estimated at up to 70% of the total land area. Since then, the forest cover has decreased progressively over time.
Rainfall is highly seasonal, falling mostly with the summer monsoon from the Bay of Bengal and South China Sea between April and October. From November to March westerly winds from continental Asia create cooler and dry conditions. January is the coldest month, and pre-monsoon spring temperatures are generally the hottest.