SRI LANKA

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SRI LANKA

This is an island of magical proportions, once known as Serendib, Taprobane, the Pearl of the Indian Ocean, and Ceylon. Discover refreshingly Sri Lanka!


Sri Lanka lies on the Indian tectonic plate, a minor plate within the Indo-Australian Plate. It is in the Indian Ocean southwest of the Bay of Bengal, between latitudes 5° and 10°N, and longitudes 79° and 82°E. Sri Lanka is separated from the Indian subcontinent by the Gulf of Mannar and Palk Strait. According to Hindu mythology, a land bridge existed between the Indian mainland and Sri Lanka. It now amounts to only a chain of limestone shoals remaining above sea level. It was reportedly passable on foot up to 1480 AD, until cyclones deepened the channel.

Proximity to equator means long daylight hours throughout the year. Sri Lanka has a tropical climate with high humidity. January is the coolest month, becoming especially cold in the highlands, and May is the hottest time of the year. Monsoon season is between May and July in the western, southern and central regions, and again between December and January in the north-eastern regions. Colombo's weather stays evenly hot and humid throughout the year, with no distinct seasons apart from two rainy seasons. Heavy monsoon rains occur between May and August, and again between October and January.


The island consists mostly of flat to rolling coastal plains, with mountains rising only in the south-central part. The highest point is Pidurutalagala, reaching 2,524 metres (8,281 ft) above sea level. The climate is tropical and warm, due to the moderating effects of ocean winds. Mean temperature ranges from 17 °C (62.6 °F) in the central highlands, where frost may occur for several days in the winter, to a maximum of 33 °C (91.4 °F) in other low-altitude areas. Average yearly temperature ranges from 28 °C (82.4 °F) to nearly 31 °C (87.8 °F). Day and night temperatures may vary by 14 °C (25.2 °F) to 18 °C (32.4 °F).


Rainfall pattern is influenced by monsoon winds from the Indian Ocean and Bay of Bengal. The "wet zone" and some of the windward slopes of the central highlands receive up to 2,500 millimetres (98.4 in) of rain each month, but the leeward slopes in the east and northeast receive little rain. Most of the east, southeast, and northern parts of the country comprise the "dry zone", which receives between 1,200 mm (47 in) and 1,900 mm (75 in) of rain annually. The arid northwest and southeast coasts receive the least amount of rain at 800 mm (31 in) to 1,200 mm (47 in) per year. Periodic squalls occur and sometimes tropical cyclones bring overcast skies and rains to the southwest, northeast, and eastern parts of the island. Humidity is typically higher in the southwest and mountainous areas and depends on the seasonal patterns of rainfall.