Tropical Cyclones In Oman
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Tropical Cyclones In Oman
The Arabian Peninsula is a peninsula between the Red Sea, the Arabian Sea, and the Persian Gulf. There are 64 known tropical cyclones that affected the peninsula, primarily Yemen and Oman. For convenience, storms are included that affected the Yemeni island of Socotra. Most of the tropical cyclones originated in the Arabian Sea, the portion of the Indian Ocean north of the equator and west of India. The remainder formed in the Bay of Bengal off India's east coast. Collectively, the 64 storms have caused at least US$8.3 billion in damage and 1,693 deaths. The strongest and most damaging cyclone was Cyclone Gonu, which caused US$4 billion in damage and 50 fatalities when it struck Oman in 2007. Tropical cyclone damage in the Arabian Peninsula is chiefly due to flooding. Climatology Within the Indian Ocean north of the equator, tropical cyclones are tracked by the India Meteorological Department (IMD), which is the officially designated Regional Specializ ...
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Gonu 2007-06-04 0900Z
Gonu (고누) or kono refers to a group of Korean traditional boardgames which are played by two players on diagrams, each taking turns to move their pieces, with the general objective to block or capture the other player's pieces. Although Gonu games are played in a manner similar to asymmetric hunt games like Fox games, Fox, Leopard hunt game, Leopard, and Tiger game, Tiger, each Gonu player starts with an equal number of pieces instead. When playing kono, a person who has a lower number starts, like janggi. The usual way of playing is to surround and detach the opponent's pieces. It is mainly used for children's educational purposes. Examples File:Five-field Kono board.svg, Five-field kono(오밭고누) File:Four-field Kono board.svg, Four-field kono(네밭고누) File:Twelve Men's Morris board.svg, Morabaraba, Gonjilgonu(참고누) File:Well Kono board.svg, Pong Hau K'i, Umul gonu(우물고누) References

Abstract strategy games Asian games Korean games Traditio ...
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India Meteorological Department
India Meteorological Department (IMD) is an Indian agency of the Ministry of Earth Sciences of the Government of India. It is the principal agency responsible for meteorological observations, weather forecasting and seismology. IMD is headquartered in Delhi and operates hundreds of observation stations across India and Antarctica. Regional offices are at Chennai, Mumbai, Kolkata, Nagpur, Guwahati and New Delhi. IMD is also one of the six Regional Specialised Meteorological Centres of the World Meteorological Organisation. It has the responsibility for forecasting, naming and distribution of warnings for tropical cyclones in the Northern Indian Ocean region, including the Malacca Straits, the Bay of Bengal, the Arabian Sea and the Persian Gulf. History In 1686, Edmond Halley published his treatise on the Indian summer monsoon, which he attributed to a seasonal reversal of winds due to the differential heating of the Asian landmass and the Indian Ocean. The first meteorologic ...
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1977 Oman Cyclone
The 1977 Oman cyclone was the deadliest tropical cyclone on record to strike Oman. The storm formed off the west coast of India in the Arabian Sea, and curved westward to reach peak winds of . The storm struck Masirah Island and later southern Oman on June 13, before dissipating the next day over Saudi Arabia. Producing wind gusts to , the storm was the strongest cyclone on record to hit the Arabian Peninsula until Cyclone Gonu hit in 2007. About 95% of Marisah Island was damaged by the strong winds, including much of the military base. The cyclone dropped of rainfall over a 24-hour period on Marisah, which was the highest daily total in the country as of 2003. Overall, the storm killed at least 105 people and left 50,000 homeless. Meteorological history On June 6, a monsoon depression formed in the Arabian Sea about south-southwest of Goa, India. It initially paralleled the Indian coastline, becoming a tropical storm on June 9 with a minimum barometric pres ...
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Cyclone Keila
Cyclonic Storm Keila () (IMD designation: ''ARB 02'', JTWC designation: ''03A'') was the first named storm Tropical cyclones and subtropical cyclones are named by various warning centers to simplify communication between forecasters and the general public regarding forecasts, watches and warnings. The names are intended to reduce confusion in the ... of the 2011 North Indian Ocean cyclone season. A weak system for much of its duration, Keila developed in the western Arabian Sea in late October 2011, amid an area of marginally favorable conditions. On November 2, it briefly organized enough to be classified as a Tropical cyclone scales#North Indian Ocean, cyclonic storm, which has maximum sustained winds of at least . Given the name Keila by the India Meteorological Department (IMD), the storm quickly moved ashore southern Oman near Salalah, and weakened while meandering over the country. The remnants soon after moved offshore, dissipating on November 4. The storm ...
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Cyclone Phet
Very Severe Cyclonic Storm Phet () was a powerful tropical cyclone that made landfall on Oman, Western India, and Pakistan. The third named cyclone of the 2010 North Indian Ocean cyclone season, 2010 cyclone season, Phet developed in the Arabian Sea on May 31 to the west of India. With conducive environmental conditions, the storm intensified to reach peak maximum sustained wind, sustained winds of on June 2, based on analysis by the India Meteorological Department (IMD). On the next day, Phet dropped heavy rainfall while moving across eastern Oman, with a peak of in Qurayyat, Oman, Qurayyat. The rains flooded arid areas and collected into wadis – normally dry river beds. Thousands of homes were wrecked across Oman. There were 24 fatalities in the country, and damage was estimated at US$780 million. After exiting Oman on June 4, Phet turned to the northeast and later to the east while continuing to weaken. The residual thunderstorms spread ahea ...
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Ras Al Hadd
Raʾs al-Ḥadd () is a village in Ash Sharqiyah district in Oman. It is on a point at the entrance to the Gulf of Oman. The region is served by Ras al Hadd Airport. Geography Al-Hajar Mountains are located to the west. The beaches at Ras al Hadd and nearby '' Ra's al-Jinz'' are known as a breeding ground for green sea turtles. Indian intelligence radar There is an Indian listening post at Ras al Hadd,"India activates first listening post on foreign soil: radars in Madagascar"
, 18 July 2007.
, .
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Dhofar Governorate
The Dhofar Governorate () is the largest of the 11 Governorates of Oman, governorates in the Oman, Sultanate of Oman in terms of area. It lies in southern Oman, on the eastern border with Yemen's Al Mahrah Governorate and the southern border with Saudi Arabia's Eastern Province, Saudi Arabia, Eastern Province. It is a rather mountainous area that covers and had a population of 416,458 in the 2020 census. Salalah is the largest city and capital of the governorate. Historically, the region was a source of frankincense. The local dialect of Arabic is Dhofari Arabic, which is distinct from that used in the rest of Oman and in Yemen. History Archaeology At ''Aybut Al-Auwal'' ("First Aybut") in Wadi Aybut (west-central Nejd), a site was discovered in 2011 containing more than 100 surface scatters of stone tools belonging to a regionally specific lithic industry, the late Nubian Complex, known previously only from Northeast Africa. Two optically stimulated Luminescence dating, lumin ...
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Salalah
Salalah () is the capital and largest city of the southern Omani Governorates of Oman, governorate of Dhofar Governorate, Dhofar. It has a population close to 331,949. Salalah is the third-largest city in the Sultanate of Oman, and the largest city in the Dhofar province. Salalah is the birthplace of former Omani List of rulers of Oman, Sultan Qaboos bin Said al Said, Qaboos bin Said. Salalah attracts many tourists from other parts of Oman and from abroad during the monsoon/''khareef'' season, from June to September. The climate of the region and the monsoon allow the city to grow some vegetables and fruits like coconut and bananas. There are many gardens within the city where these vegetables and fruits grow. History Salalah currently is and was the traditional capital of Dhofar, which reached the peak of prosperity in the 13th century thanks to the incense trade. Later it decayed, and in the 19th century it was absorbed by the Sultanate of Muscat and Oman. Between 1932 and 1 ...
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Masirah Island
Masirah Island (), also referred to as Mazeira Island, is an island off the east coast of mainland Oman in the Arabian Sea, and the largest island of the country. Administratively, it forms one of the five Provinces of Oman, provinces (''Wilayah'', plural ''Wilayat'') of the Ash Sharqiyah South Governorate, namely ''Wilāyat Maṣīrah'' (); previously it was a province of the Ash Sharqiyah Region (Oman), Ash Sharqiyah Region. Masirah is long north–south, between wide, with an area of about 649 km2, and a population estimated at 12,000 in 12 villages mainly in the north of the island (9,292 as of the census of 2003, of which were 2,311 foreigners). It is divided from the mainland by the Masirah Channel. Most of the island's interior is deserted, with access to the island possible by ferry on National Ferries Company (NFC) or smaller privately owned ferries for cars and passengers. Salam Air also flies to Masirah weekly. The principal village of Wilayat Masirah is ''Ra� ...
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Arabian Peninsula (orthographic Projection)
The Arabian Peninsula (, , or , , ) or Arabia, is a peninsula in West Asia, situated north-east of Africa on the Arabian plate. At , comparable in size to India, the Arabian Peninsula is the largest peninsula in the world. Geographically, the Arabian Peninsula comprises Bahrain, Kuwait, Oman, Qatar, Saudi Arabia, the United Arab Emirates (UAE) and Yemen, as well as southern Iraq and Jordan. The largest of these is Saudi Arabia. In the Roman era, the Sinai Peninsula was also considered a part of Arabia. The Arabian Peninsula formed as a result of the rifting of the Red Sea between 56 and 23 million years ago, and is bordered by the Red Sea to the west and south-west, the Persian Gulf and the Gulf of Oman to the north-east, the Levant and Mesopotamia to the north and the Arabian Sea and the Indian Ocean to the south-east. The peninsula plays a critical geopolitical role in the Arab world and globally due to its vast reserves of oil and natural gas. Before the modern era, ...
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Monsoon
A monsoon () is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation but is now used to describe seasonal changes in Atmosphere of Earth, atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator. Usually, the term monsoon is used to refer to the Wet season, rainy phase of a seasonally changing pattern, although technically there is also a dry phase. The term is also sometimes used to describe locally heavy but short-term rains. The major monsoon systems of the world consist of the Monsoon#Africa (West African and Southeast African), West African, Asian–Australian monsoon, Australian, the North American monsoon, North American, and South American monsoons. The term was first Glossary of the British Raj, used in English in British India and neighboring countries to refer to the big seasonal winds blowin ...
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Sea Surface Temperature
Sea surface temperature (or ocean surface temperature) is the ocean temperature, temperature of ocean water close to the surface. The exact meaning of ''surface'' varies in the literature and in practice. It is usually between and below the sea surface. Sea surface temperatures greatly modify air masses in the Atmosphere of Earth, Earth's atmosphere within a short distance of the shore. The thermohaline circulation has a major impact on average sea surface temperature throughout most of the world's oceans. Warm sea surface temperatures can develop and Tropical cyclogenesis, strengthen cyclones over the ocean. Tropical cyclones can also cause a cool wake. This is due to turbulent mixing of the upper of the ocean. Sea surface temperature changes during the day. This is like the air above it, but to a lesser degree. There is less variation in sea surface temperature on breezy days than on calm days. Coastal sea surface temperatures can cause offshore winds to generate upwelling ...
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