1992 North Indian Ocean Cyclone Season
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1992 North Indian Ocean Cyclone Season
The 1992 North Indian Ocean cyclone season was unofficially the most active year on record for the basin, with 10 tropical storms developing, according to the Joint Typhoon Warning Center (JTWC). There are two main seas in the North Indian Ocean – the Bay of Bengal to the east of the Indian subcontinent – and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the JTWC releases unofficial advisories. An average of four to six storms form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD. Overall, there was a total of 12 depressions, of which 7 became cyclonic storms, and 1 further strengthened to a very severe cyclonic storm. These totals were slightly above the long-term average of 5.4 cyclonic storms for the basin. In contrast ...
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Cyclone Forrest (1992)
Extremely Severe Cyclonic Storm Forrest, also referred to as Tropical Storm Forrest while in the western Pacific basin before its Thai crossover, was a powerful tropical cyclone that prompted the evacuation of 600,000 people in Bangladesh in late November 1992. Originating from an area of disturbed weather near the Caroline Islands on November 9, Forrest was classified as a tropical depression three days later over the South China Sea. Tracking generally west, the system steadily organized into a tropical storm, passing Vietnam to the south, before striking Thailand along the Malay Peninsula on November 15. Once over the Bay of Bengal, Forrest turned northward on November 17 and significantly intensified. It reached its peak intensity on November 20 as a Category 4-equivalent cyclone on the Saffir–Simpson hurricane scale with winds of 230 km/h (145 mph). Hostile environmental conditions soon affected the cyclone as it turned abruptly ...
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Category 1 Hurricane
Category 1 can refer to: *Category 1 cable, an electrical standard for communications wiring * Category 1 tropical cyclone, on any of the Tropical cyclone scales * Cat11egory 1 pandemic, on the Pandemic Severity Index, an American influenza pandemic with a case-fatality ratio of less than 0.1% * Category 1 winter storm, on the Northeast Snowfall Impact Scale and the Regional Snowfall Index ** Any of several winter storms listed at list of Northeast Snowfall Impact Scale winter storms * Classification of non-silicate minerals#Category 01, Category 01 non-silicate mineral - native element minerals See also

* Class 1 (other) - class/category equivalence (for labeling) * Type 1 (other) - type/category equivalence (for labeling) * Group 1 (other) - group/category equivalence (for labeling) * Category I (other) - Roman/Arabic numbering equivalence {{disambiguation ...
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Yemen
Yemen (; ar, ٱلْيَمَن, al-Yaman), officially the Republic of Yemen,, ) is a country in Western Asia. It is situated on the southern end of the Arabian Peninsula, and borders Saudi Arabia to the Saudi Arabia–Yemen border, north and Oman to the Oman–Yemen border, northeast and shares maritime borders with Eritrea, Djibouti, and Somalia. Yemen is the second-largest Arabs, Arab sovereign state in the peninsula, occupying , with a coastline stretching about . Its constitutionally stated Capital city, capital, and largest city, is Sanaa. As of 2021, Yemen has an estimated population of some 30.4 million. In ancient times, Yemen was the home of the Sabaeans, a trading state that included parts of modern-day Ethiopia and Eritrea. Later in 275 AD, the Himyarite Kingdom was influenced by Judaism. Christianity arrived in the fourth century. Islam spread quickly in the seventh century and Yemenite troops were crucial in the early Islamic conquests. Several Dynasty, dynasties ...
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Wind Shear
Wind shear (or windshear), sometimes referred to as wind gradient, is a difference in wind speed and/or direction over a relatively short distance in the atmosphere. Atmospheric wind shear is normally described as either vertical or horizontal wind shear. Vertical wind shear is a change in wind speed or direction with a change in altitude. Horizontal wind shear is a change in wind speed with a change in lateral position for a given altitude. Wind shear is a microscale meteorological phenomenon occurring over a very small distance, but it can be associated with mesoscale or synoptic scale weather features such as squall lines and cold fronts. It is commonly observed near microbursts and downbursts caused by thunderstorms, fronts, areas of locally higher low-level winds referred to as low-level jets, near mountains, radiation inversions that occur due to clear skies and calm winds, buildings, wind turbines, and sailboats. Wind shear has significant effects on the control of a ...
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Tropical Cyclone Formation Alert
A Tropical Cyclone Formation Alert (TCFA) is a bulletin released by the U.S. Navy-operated Joint Typhoon Warning Center in Honolulu, Hawaii or the Fleet Weather Center in Norfolk, Virginia, warning of the possibility of a tropical cyclone forming from a tropical disturbance that has been monitored. Such alerts are generally always issued when it is fairly certain that a tropical cyclone will form and are not always released before cyclone genesis, particularly if the cyclone appears suddenly. The TCFA consists of several different checks that are performed by the on-duty meteorologist of the system and its surroundings. If the condition being checked is met, a certain number of points are given to the system. Parts of the TCFA Section 1 The first section of the TCFA contains information on the area of the alert as well as the estimated center of the circulation. The estimated maximum sustained winds are provided as well. Section 2 The second section generally contains more specif ...
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Atmospheric Convection
Atmospheric convection is the result of a parcel-environment instability, or temperature difference layer in the atmosphere. Different lapse rates within dry and moist air masses lead to instability. Mixing of air during the day which expands the height of the planetary boundary layer leads to increased winds, cumulus cloud development, and decreased surface dew points. Moist convection leads to thunderstorm development, which is often responsible for severe weather throughout the world. Special threats from thunderstorms include hail, downbursts, and tornadoes. Overview There are a few general archetypes of atmospheric instability that are used to explain convection (or lack thereof). A necessary (but not sufficient) condition for convection is that the environmental lapse rate (the rate of decrease of temperature with height) is steeper than the lapse rate experienced by a rising parcel of air. When this condition is met, upward-displaced air parcels can become buoyant and th ...
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Radio Rangoon
Radio is the technology of signaling and communicating using radio waves. Radio waves are electromagnetic waves of frequency between 30 hertz (Hz) and 300  gigahertz (GHz). They are generated by an electronic device called a transmitter connected to an antenna which radiates the waves, and received by another antenna connected to a radio receiver. Radio is very widely used in modern technology, in radio communication, radar, radio navigation, remote control, remote sensing, and other applications. In radio communication, used in radio and television broadcasting, cell phones, two-way radios, wireless networking, and satellite communication, among numerous other uses, radio waves are used to carry information across space from a transmitter to a receiver, by modulating the radio signal (impressing an information signal on the radio wave by varying some aspect of the wave) in the transmitter. In radar, used to locate and track objects like aircraft, ships, spacecraft ...
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Ramree
Ramree or Ramarwaddy ( my, ရမ်းဗြဲမြို့, ) also known as Yanbye is a town in Kyaukpyu District, Rakhine State, Myanmar. Ramree (locally pronounced Ram Bray) is situated on Ramree Island. Ramree is the capital of the township of the same name and former capital of the district of Ramree (until 1852 ). It is close to the east coast of the Ramree island, about north of the Tan River. The population of Ramree (Yanbye) Urban area is 9,581 as of 2014, while Ramree Township's population is 97,891. Etymology The name "Ramree" (ရမ်းဗြဲ) is derived from the former name of island: Ramarwaddy (ရမ္မာဝတီ) which meant Pleasant Region (Rammar= Pleasant) (Wati = Region). The administrative town of Rammar Wati was called "Rammar Wati Pri Myo" and then acronymic way, town's name was shorten to Ram Pri Myo (ရမ်ပြည်မြို့) which was heard by Portuguese firstly landed Europeans to this town as Rama Ree or Rama Ri later it w ...
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Kyaukpyu
Kyaukpyu ( my, ကျောက်ဖြူမြို့ ; also spelt Kyaukphyu) is a major town in Rakhine State, in western Myanmar. It is located on the north western corner of Yanbye Island on Combermere Bay, and is 250 miles (400 km) north-west of Yangon. It is the principal town of Kyaukpyu Township and Kyaukpyu District. The town is situated on a superb natural harbor which connects the rice trade between Calcutta and Yangon. The estimated population in 1983 was 19,456 inhabitants. The population of Kyaukpyu Urban area is 20,866 as of 2014, while Kyaukpyu Township's population is 165,352. Etymology The name Kyaukpyu (lit. "white rock") is the Burmese pronunciation. In the local Rangbre pronunciation of the natives of Kyaukpyu and in standard Arakanese, the town's name is pronounced "Kyaukpru". The old Kyaukpyu is situated 7 miles from the present town where two colossal white rocks exist. History The place where the present town is, was originally a sm ...
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Manaung
Manaung ( my, မာန်အောင်မြို့) is a town in Rakhine State, Myanmar (Burma) on Cheduba Island. It lies on the left bank of a river in the north-east of the island. The town is served by Manaung Airport. Climate References External linksmanaung.comMaplandia.com
Township capitals of Myanmar Populated places in Rakhine State {{Burma-geo-stub ...
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Thandwe
Thandwe ("Thandway" in Arakanese; ; formerly Sandoway) is a town and major seaport in Rakhine State, the westernmost part of Myanmar. Thandwe is very ancient, and is said to have been at one time the capital of Rakhine State, then called Arakan. The district has an area of . The area is mountainous, and spurs of the Arakan Mountains reach the coast. Some of the peaks in the north are over high. The streams are only mountain torrents to within a few miles of the coast; the mouth of the Khwa forms a good anchorage for small boats. The rocks in the Arakan Range and its spurs are metamorphic, and include clay, slates, ironstone and indurated sandstone; towards the south, ironstone, trap and rocks of basaltic character are common; veins of steatite and white fibrous quartz are also found. Between 1961 and 1990, the mean annual rainfall was . Nearby Ngapali Beach is popular among tourists. Climate Thandwe has a tropical monsoon climate (Köppen climate classification ''Am''). Tempera ...
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Taungup
Taungup, Toungup or Toungok ( my, တောင်ကုတ်မြို့) is a principal town of the Taungup Township in the Rakhine State of westernmost part of Myanmar. As of May 2020, there is one case of COVID-19, one of two cases in not only Thandwe township, but the whole Rakhine State.It got 29.1 inches of rainfall on 21 July 2011. It was record breaking and there was severe flooding. The population of Taungup (Toungup) Urban area is 28,652 as of 2014, while Taungup Township Taungup or Toungup Township ( my, တောင်ကုတ်မြို့နယ်) is a coastal township of Thandwe District in the Rakhine State of Myanmar. The administrative centre and principal town is Toungup Taungup, Toungup or Toungo ...'s population is 114,437. There are 2 Universities in Rakhine State,One located in Sittwe( Sittwe University) and another One located in Taungup(Taungup University).https://www.gnlm.com.mm/sac-member-union-ministers-attend-opening-ceremony-of-taungup ...
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