Maavaidhoo | |
|---|---|
  Maavaidhoo Location in Maldives | |
| Coordinates: 06°30′55″N73°03′04″E / 6.51528°N 73.05111°E Coordinates: 06°30′55″N73°03′04″E / 6.51528°N 73.05111°E | |
| Country | Maldives |
| Geographic atoll | Thiladhummathi Atoll |
| Administrative atoll | Haa Dhaalu Atoll |
| Distance to Malé | 262.67 km (163.22 mi) |
| Government | |
| • Island Chief | Abdur-Rahman Moosa |
| Dimensions | |
| • Length | 0.870 km (0.541 mi) |
| • Width | 0.600 km (0.373 mi) |
| Population | |
| • Total | 525 |
| Time zone | UTC+05:00 (MST) |
Maavaidhoo (Dhivehi: މާވައިދޫ) is one of the inhabited islands of Haa Dhaalu Atoll administrative division and geographically part of Thiladhummathi Atoll in the north of the Maldives.
Haa Dhaalu Atoll is the code name based on the letters of the Maldivian alphabet commonly used to refer to the administrative division officially known as South Thiladhunmathi Atoll in the Maldives.
The Maldives, officially the Republic of Maldives, is a country in South Asia, located in the Arabian Sea of the Indian Ocean. It lies southwest of Sri Lanka and India, about 1,000 kilometres (620 mi) from the Asian continent. The chain of 26 atolls stretches from Ihavandhippolhu Atoll in the north to Addu Atoll in the south. Comprising a territory spanning roughly 298 square kilometres (115 sq mi), the Maldives is one of the world's most geographically dispersed sovereign states as well as the smallest Asian country by land area and population, with around 427,756 inhabitants. Malé is the capital and the most populated city, traditionally called the "King's Island" for its central location.
The island was severely damaged by the great cyclone of 1821 that hit the northern atolls of the Maldives.
In meteorology, a cyclone is a large scale air mass that rotates around a strong center of low atmospheric pressure. Cyclones are characterized by inward spiraling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale. Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes and dust devils lie within smaller mesoscale. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars and Neptune. Cyclogenesis is the process of cyclone formation and intensification. Extratropical cyclones begin as waves in large regions of enhanced mid-latitude temperature contrasts called baroclinic zones. These zones contract and form weather fronts as the cyclonic circulation closes and intensifies. Later in their life cycle, extratropical cyclones occlude as cold air masses undercut the warmer air and become cold core systems. A cyclone's track is guided over the course of its 2 to 6 day life cycle by the steering flow of the subtropical jet stream.
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