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2008 North Indian Ocean Cyclone Season
The 2008 North Indian cyclone season was one of the most disastrous tropical cyclone seasons in modern history, with tropical cyclones leaving more than 140,000 people dead and causing more than US$15 billion in damage, making it the costliest season in the North Indian Ocean, until it was made second in 2020. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. 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 Joint Typhoon Warning Center 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 occurr ...
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Cyclone Nargis
Extremely Severe Cyclonic Storm Nargis ( my, နာဂစ်, ur, نرگس ) was an extremely destructive and deadly tropical cyclone that caused the worst natural disaster in the recorded history of Myanmar during early May 2008. The cyclone made landfall in Myanmar on Friday, 2 May 2008, sending a storm surge 40 kilometres up the densely populated Irrawaddy delta, causing catastrophic destruction and at least 138,373 fatalities. The Labutta Township alone was reported to have 80,000 dead, with about 10,000 more deaths in Bogale. There were around 55,000 people missing and many other deaths were found in other towns and areas, although the Myanmar government's official death toll may have been under-reported, and there have been allegations that government officials stopped updating the death toll after 138,000 to minimise political fallout. The feared 'second wave' of fatalities from disease and lack of relief efforts never materialised. Damage was at $12 billion, making Nargi ...
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100th Meridian East
The meridian 100° east of Greenwich is a line of longitude that extends from the North Pole across the Arctic Ocean, Asia, the Indian Ocean, the Southern Ocean, and Antarctica to the South Pole. The 100th meridian east forms a great circle with the 80th meridian west. From Pole to Pole Starting at the North Pole and heading south to the South Pole The South Pole, also known as the Geographic South Pole, Terrestrial South Pole or 90th Parallel South, is one of the two points where Earth's axis of rotation intersects its surface. It is the southernmost point on Earth and lies antipod ..., the 100th meridian east passes through: : {{geographical coordinates, state=collapsed e100 meridian east ...
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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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Intertropical Convergence Zone
The Intertropical Convergence Zone (ITCZ ), known by sailors as the doldrums or the calms because of its monotonous windless weather, is the area where the northeast and the southeast trade winds converge. It encircles Earth near the thermal equator though its specific position varies seasonally. When it lies near the geographic Equator, it is called the near-equatorial trough. Where the ITCZ is drawn into and merges with a monsoonal circulation, it is sometimes referred to as a monsoon trough, a usage that is more common in Australia and parts of Asia. Meteorology The ITCZ was originally identified from the 1920s to the 1940s as the ''Intertropical Front'' (''ITF''), but after the recognition in the 1940s and the 1950s of the significance of wind field convergence in tropical weather production, the term ''Intertropical Convergence Zone'' (''ITCZ'') was then applied. The ITCZ appears as a band of clouds, usually thunderstorms, that encircle the globe near the Equator. In the ...
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Cyclone Nisha (2008)
Cyclonic Storm Nisha ( IMD designation: BOB 07, JTWC designation: 06B) was a fairly weak but catastrophic tropical cyclone that struck Sri Lanka, and India which killed over 200. It was the ninth tropical cyclone of the 2008 North Indian Ocean cyclone season, and the seventh tropical cyclone in the Bay of Bengal that year. Meteorological history On November 24 an area of low pressure formed over land in Sri Lanka. Later that day the Joint Typhoon Warning Center assessed the low-pressure area's chance of becoming a significant tropical cyclone within 24 hours as 'poor', due to the minimal convection near the low-level circulation center. The next morning the JTWC issued a Tropical Cyclone Formation Alert on the low-pressure area, stating it had a 'good' chance of becoming a significant tropical cyclone within 24 hours, as the Low Level Circulation Center was moving into the Bay of Bengal. Two hours later the IMD upgraded the area of low pressure to Depression BOB 07. Three ...
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Cyclone Rashmi
Cyclonic Storm Rashmi ( IMD designation: BOB 05, JTWC designation: 04B) was the seventh tropical cyclone of the 2008 North Indian Ocean cyclone season and second cyclonic storm, as well as the fifth tropical cyclone in the Bay of Bengal that year. A fairly weak tropical cyclone, it caused some notable damage in Bangladesh and India. An area of low pressure formed within the Bay of Bengal on October 24. It was designated as Depression BOB 05 the next day by the India Meteorological Department. The depression was declared a deep depression early on October 26, whilst the Joint Typhoon Warning Center designated the depression as Cyclone 04B later that day with wind speeds equivalent to a tropical storm. Later that day, the IMD upgraded the deep depression into a cyclonic storm and named it as Rashmi. Rashmi then reached both its peak one- and three-minute sustained wind speeds, as it made landfall on the Bangladesh coast late on October 26. Early the next day the JTWC issued its final ...
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2008 Yemen Cyclone
Deep Depression ARB 02 was a weak yet costly tropical cyclone which caused extensive damage and loss of life in Yemen. The sixth tropical cyclone and third deep depression of the 2008 North Indian Ocean cyclone season, ARB 02 formed in the Arabian Sea on October 19 from the same broader system which would spawn Moderate Tropical Storm Asma in the southern Indian Ocean around that time. Moving generally westward, the depression failed to intensify further, reaching maximum sustained winds of . It would weaken, becoming a remnant low on October 23. Later that day, the system's remnants would made landfall near Ash Shihr in eastern Yemen. The storm sent a plume of moisture throughout the Arabian Peninsula, contributing to dust storms as far north as Iraq. However, the effects were most severe in Yemen, becoming the second-worst natural disaster in the country after deadly floods in 1996. The storm dropped heavy rainfall in a normally arid region, reaching around , which cau ...
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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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Sri Lanka
Sri Lanka (, ; si, ශ්‍රී ලංකා, Śrī Laṅkā, translit-std=ISO (); ta, இலங்கை, Ilaṅkai, translit-std=ISO ()), formerly known as Ceylon and officially the Democratic Socialist Republic of Sri Lanka, is an island country in South Asia. It lies in the Indian Ocean, southwest of the Bay of Bengal, and southeast of the Arabian Sea; it is separated from the Indian subcontinent by the Gulf of Mannar and the Palk Strait. Sri Lanka shares a maritime border with India and Maldives. Sri Jayawardenepura Kotte is its legislative capital, and Colombo is its largest city and financial centre. Sri Lanka has a population of around 22 million (2020) and is a multinational state, home to diverse cultures, languages, and ethnicities. The Sinhalese are the majority of the nation's population. The Tamils, who are a large minority group, have also played an influential role in the island's history. Other long established groups include the Moors, the Burghers ...
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Bangladesh
Bangladesh (}, ), officially the People's Republic of Bangladesh, is a country in South Asia. It is the eighth-most populous country in the world, with a population exceeding 165 million people in an area of . Bangladesh is among the most densely populated countries in the world, and shares land borders with India to the west, north, and east, and Myanmar to the southeast; to the south it has a coastline along the Bay of Bengal. It is narrowly separated from Bhutan and Nepal by the Siliguri Corridor; and from China by the Indian state of Sikkim in the north. Dhaka, the capital and largest city, is the nation's political, financial and cultural centre. Chittagong, the second-largest city, is the busiest port on the Bay of Bengal. The official language is Bengali, one of the easternmost branches of the Indo-European language family. Bangladesh forms the sovereign part of the historic and ethnolinguistic region of Bengal, which was divided during the Partition of India in ...
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Burmese Kyat
The kyat (, or ; my, ကျပ် ; ISO 4217 code MMK) is the currency of Myanmar (Burma). The typical notation for the kyat is "K" (singular) and "Ks." (plural), placed before the numerals followed by " /-" The term ''kyat'' derives from the ancient Burmese unit ''kyattha'' ( my, ကျပ်သား), equal to 16.3 (16.329324593) grams of silver. Current MMK exchange rates From 2001 to 2012, the official exchange rate varied between Ks. 5/75 and Ks. 6/70 per US dollar (Ks. 8/20 to Ks. 7/- per euro). However, the street rate (black market rate), which more accurately took into account the standing of the national economy, has varied from Ks.750/- to Ks.1,335/- per USD (Ks.985/- to Ks.1,475/- per EUR). The black market exchange rates (USD to MMK) decrease during the peak of the tourist season in Burma (December to January). On 2 April 2012, the Central Bank of Myanmar announced that the value of the kyat against the US dollar would float, setting an in ...
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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. There is a suggestion that climate change may be increasing the hazard of storm surges. Some theorize that as extreme weather becomes more intense and sea level rises due to climate change, storm surge is expected to cause more risk to coastal populations. Communities and governments can adapt by building hard infrastructure, like surge barriers, soft infrastructure, ...
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