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1994 North Indian Ocean Cyclone Season
The 1994 North Indian Ocean cyclone season was a below-average year in which eight tropical cyclones affected seven countries bordering the North Indian Ocean. The India Meteorological Department tracks all tropical cyclones in the basin, north of the equator. The first system developed on March 21 in the Bay of Bengal, the first March storm in the basin since 1938. The second storm was the most powerful cyclone of the season, attaining maximum sustained winds of in the northern Bay of Bengal. Making landfall near the border of Bangladesh and Myanmar, the cyclone killed 350 people and left US$125 million in damage. A storm in June originated over western India and crossed the northern Arabian Sea, later striking Oman. In August, a deep depression moved across much of India into Pakistan. Another deep depression in October killed 38 people in southeastern India. In late October, a storm crossed over Chennai in southern India, leaving US$115 million in da ...
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1994 Bangladesh Cyclone
The 1994 Bangladesh cyclone was a powerful tropical cyclone in the Bay of Bengal. The cyclone closely followed the path, strength, and time of year of a 1991 Bangladesh cyclone, deadly cyclone in 1991 that killed more than 138,000 people. The 1994 cyclone formed on April 29 as a tropical cyclone scales#North Indian Ocean, depression, which organized and intensified significantly over the subsequent few days. On May 2, the cyclone attained maximum sustained wind, winds of , according to the India Meteorological Department (IMD). That day, the storm made landfall in southeastern Bangladesh, and rapidly weakened over land, before dissipating on May 3. Ahead of the storm's landfall, about 450,000 people evacuated to storm shelters built since the 1991 storm. Upon moving ashore, the cyclone dropped of precipitation and produced winds of in Teknaf Upazila. Total storm damage was estimated at $125 million (1994 United States dollar, USD). The cyclone ...
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Joint Typhoon Warning Center
The Joint Typhoon Warning Center (JTWC) is a joint United States Navy – United States Air Force command in Pearl Harbor, Hawaii. The JTWC is responsible for the issuing of tropical cyclone warnings in the North-West Pacific Ocean, South Pacific Ocean, and Indian Ocean for all branches of the U.S. Department of Defense and other U.S. government agencies. Their warnings are intended primarily for the protection of U.S. military ships and aircraft, as well as military installations jointly operated with other countries around the world. Its U.S. Navy components are aligned with the Naval Meteorology and Oceanography Command. History The origins of the Joint Typhoon Warning Center (JTWC) can be traced back to June 1945, when the Fleet Weather Center/Typhoon Tracking Center was established on the island of Guam, after multiple typhoons, including Typhoon Cobra of December 1944 and Typhoon Connie in June 1945, had caused a significant loss of men and ships. At this time th ...
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Gudluru
Gudluru is a Mandal in Nellore district of the Indian state of Andhra Pradesh. It is the mandal headquarters of Gudluru mandal in Kandukur revenue division. Politics Kandukur is an Assembly Constituency An electoral (congressional, legislative, etc.) district, sometimes called a constituency, riding, or ward, is a geographical portion of a political unit, such as a country, state or province, city, or administrative region, created to provi ... in Andhra Pradesh. References {{reflist Villages in Prakasam district Mandal headquarters in Prakasam district ...
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Oman
Oman, officially the Sultanate of Oman, is a country located on the southeastern coast of the Arabian Peninsula in West Asia and the Middle East. It shares land borders with Saudi Arabia, the United Arab Emirates, and Yemen. Oman’s coastline faces the Arabian Sea to the southeast and the Gulf of Oman on the northeast. The exclaves of Madha and Musandam Governorate, Musandam are surrounded by the United Arab Emirates on their land borders, while Musandam’s coastal boundaries are formed by the Strait of Hormuz and the Gulf of Oman. The capital and largest city is Muscat. With a population of approximately 5.46 million and an area of 309,500 km2 (119,500 sq mi), Oman is the Countries with highest population, 123rd most-populous country. From the 18th century, the Omani Sultanate was Omani Empire, an empire, competing with the Portuguese Empire, Portuguese and British Empire, British empires for influence in the Persian Gulf and the Indian Ocean. At its peak in the 19th ce ...
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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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Ratnagiri
Ratnagiri (IAST:Ratnāgirī ; �ət̪n̪aːɡiɾiː is a port city on the Arabian Sea coast in Ratnagiri District in southwestern Maharashtra, India. The district is part of Konkan division of Maharashtra. The city is known for the Hapus or Alphonso mangoes and is colloquially referred to as the Mango City. Ratnagiri is the birthplace of Indian independence activist Lokmanya Tilak. Thibaw, the last king of Burma, alongside his consort Supayalat and two infant daughters were exiled to a two-storied brick mansion in Ratnagiri. The building is now known as Thibaw Palace. Geography Ratnagiri is located at . It has an average elevation of 11 meters (36 feet). The Sahyadri mountains border Ratnagiri to the east. Climate Transport Road Ratnagiri is well connected to the other parts of the state and country by National Highways & State Highways. National Highways NH 66 ( Panvel – Edapally), NH 166 (Ratnagiri – Nagpur) and Coastal Highway (Rewas – Reddy) ...
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Maharashtra
Maharashtra () is a state in the western peninsular region of India occupying a substantial portion of the Deccan Plateau. It is bordered by the Arabian Sea to the west, the Indian states of Karnataka and Goa to the south, Telangana to the southeast and Chhattisgarh to the east, Gujarat and Madhya Pradesh to the north, and the Indian union territory of Dadra and Nagar Haveli and Daman and Diu to the northwest. Maharashtra is the second-most populous state in India, the third most populous country subdivision in South Asia and the fourth-most populous in the world. The state is divided into 6 divisions and 36 districts. Mumbai is the capital of Maharashtra due to its historical significance as a major trading port and its status as India's financial hub, housing key institutions and a diverse economy. Additionally, Mumbai's well-developed infrastructure and cultural diversity make it a suitable administrative center for the state, and the most populous urban are ...
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Thermal Low
Thermal lows, or heat lows, are non- frontal low-pressure areas that occur over the continents in the subtropics during the warm season, as the result of intense heating when compared to their surrounding environments.Glossary of Meteorology (2009)Thermal Low. American Meteorological Society. Retrieved on 2009-03-02. Thermal lows occur near the Sonoran Desert, on the Mexican Plateau, in California's Great Central Valley, in the Sahara, in the Kalahari, over north-west Argentina, in South America, over the Kimberley region of north-west Australia, over the Iberian Peninsula, and over the Tibetan Plateau. On land, intense, rapid solar heating of the Earth's surface causes the heating of the lowest layers of the atmosphere, via re-radiated energy in the infrared spectrum. The hotter air is less dense than surrounding cooler air and rises, leading to the formation of a low-pressure area. Elevated areas can enhance the strength of the thermal low because they warm more quickly than ...
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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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Storm Surge
A storm surge, storm flood, tidal surge, or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low-pressure weather systems, such as cyclones. It is measured as the rise in water level above the normal tidal level, and does not include waves. The main meteorological factor contributing to a storm surge is high-speed wind pushing water towards the coast over a long fetch. Other factors affecting storm surge severity include the shallowness and orientation of the water body in the storm path, the timing of tides, and the atmospheric pressure drop due to the storm. As extreme weather becomes more intense and the sea level rises due to climate change, storm surges are expected to cause more risk to coastal populations. Communities and governments can adapt by building hard infrastructure, like surge barriers, soft infrastructure, like coastal dunes or mangroves, improving coastal construction practices and building social strat ...
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Rohingya Refugees In Bangladesh
Rohingya refugees in Bangladesh are forcibly displaced Myanmar nationals from Rakhine State who are living in Bangladesh. The Rohingya people have experienced ethnic and religious persecution in Myanmar for decades. Hundreds of thousands have fled to other countries in Southeast Asia, including Malaysia, Indonesia, and Philippines. The majority have sought refuge in Bangladesh. In Bangladesh, there are two officially registered refugee camps located in Ukhiya (sub-district) and Teknaf (sub-district) in Cox's Bazar District, Cox's Bazar district. Violence in Myanmar has escalated in recent years, so the number of Rohingya refugees in Bangladesh has increased rapidly. According to the UN Refugee Agency (UNHCR), more than 723,000 Rohingya have fled to Bangladesh since 25 August 2017. On 28 September 2018, at the 73rd United Nations General Assembly (UNGA), former Bangladeshi Prime Minister Sheikh Hasina said there were 1.1 million Rohingya refugees in Bangladesh by that time. Overcro ...
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1991 Bangladesh Cyclone
The 1991 Bangladesh Cyclone has been noted as one of the deadliest tropical cyclones in recorded history. It was also one of the most powerful cyclones in the Indian Ocean. Forming out of a large area of convection over the Bay of Bengal on April 24, the tropical cyclone initially developed gradually while meandering over the southern Bay of Bengal. On April 28, the storm began to accelerate northeastwards under the influence of the southwesterlies, and rapidly intensified to super cyclonic storm strength near the coast of Bangladesh on April 29. After making landfall in the Chittagong district of southeastern Bangladesh with winds of around , the cyclone rapidly weakened as it moved through northeastern India, degenerating into a remnant low over the Yunnan province in western China. One of the most powerful tropical cyclones ever recorded in the basin, the tropical cyclone caused a 6.1 m (20 ft) storm surge, which inundated the coastline, causing at least 1 ...
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