Geography and climate of Srilanka

Geography of Sri Lanka

The island of Sri Lanka lies in the Indian Ocean, to the southwest of the Bay of Bengal and to the southeast of the Arabian Sea. It is separated from the Indian subcontinent by the Gulf of Mannar and the Palk Strait. According to Hindu mythology, a land bridge to the Indian mainland, known as Rama's Bridge, was constructed during the time of Rama by the vanara architect Nala. Often referred to as Adam's Bridge, it now amounts to only a chain of limestone shoals remaining above sea level. According to temple records, this natural causeway was formerly complete, but was breached by a violent storm (probably a cyclone) in 1480. The width of the Palk Strait is small enough for the coast of Sri Lanka to be visible from the furthest point near the Indian town of Rameswaram. The pear-shaped island consists mostly of flat-to-rolling coastal plains, with mountains rising only in the south-central part. Amongst these are Sri Pada and the highest point Pidurutalagala (also known as Mt Pedro), at 2,524 meters (8,281 ft). The Mahaweli ganga (Mahaweli river) and other major rivers provide fresh water.
Topographical map of Sri Lanka.
Topographical map of Sri Lanka.

Climate of Sri Lanka


Sri Lanka's climate can be described as tropical, and quite hot. Its position between 5 and 10 north latitude endows the country with a warm climate, moderated by ocean winds and considerable moisture. The mean temperature ranges from a low of 16°C in Nuwara Eliya in the Central Highlands (where frost may occur for several days in the winter) to a high of 32° C in Trincomalee on the northeast coast (where temperatures may reach 38 °C). The average yearly temperature for the country as a whole ranges from 28 to 30 °C. Day and night temperatures may vary by 4 to 7. In January, the coolest month, many people wear coats and sweaters in the highlands and elsewhere. May, the hottest period, precedes the summer monsoon rains. The rainfall pattern is influenced by the monsoon winds of the Indian Ocean and Bay of Bengal, which encounter the slopes of the Central Highlands, they unload heavy rains on the mountain slopes and the southwestern sector of the island. Some of the windward slopes receive up to 2500 mm of rain per month, but the leeward slopes in the east and northeast receive little rain. Periodic squalls occur and sometimes tropical cyclones bring overcast skies and rains to the southwest, northeast, and eastern parts of the island. Between December to March, monsoon winds come from the northeast, bringing moisture from the Bay of Bengal. Humidity is typically higher in the southwest and mountainous areas and depends on the seasonal patterns of rainfall. At Colombo, for example, daytime humidity stays above 70% all year, rising to almost 90 percent during the monsoon season in June. Anuradhapura experiences a daytime low of 60% during the monsoon month of March, but a high of 79% during the November and December rains. In the highlands, Kandy's daytime humidity usually ranges between 70 and 79%.