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|Bay of Bengal|
Map of Bay of Bengal
|Location||South Asia and Southeast Asia|
|Primary inflows||Indian Ocean|
|Max. length||2,090 km (1,300 mi)|
|Max. width||1,610 km (1,000 mi)|
|Surface area||2,600,000 km2 (1,000,000 sq mi)|
|Average depth||2,600 m (8,500 ft)|
|Max. depth||4,694 m (15,400 ft)|
The Bay of Bengal is the northeastern part of the Indian Ocean, bounded on the west and northwest by India, on the north by Bangladesh, and on the east by Myanmar and the Andaman and Nicobar Islands of India. Its southern limit is a line between Sangaman Kanda, Sri Lanka, and the north westernmost point of Sumatra, Indonesia. It is the largest water region called a bay in the world. There are countries dependent on the Bay of Bengal in South Asia and Southeast Asia. During the existence of British India, it was named as the Bay of Bengal after the historic Bengal region. At the time, the Port of Kolkata served as the gateway to the Crown rule in India. Cox's Bazar, the longest sea beach in the world and Sundarbans, the largest mangrove forest and the natural habitat of the Bengal tiger, are located along the bay.
The Bay of Bengal occupies an area of 2,600,000 square kilometres (1,000,000 sq mi). A number of large rivers flow into the Bay of Bengal: the Ganges–Hooghly, the Padma, the Brahmaputra–Jamuna, the Barak–Surma–Meghna, the Irrawaddy, the Godavari, the Mahanadi, the Brahmani, the Baitarani, the Krishna and the Kaveri.
Important ports include Krishnapatnam, Chennai, Ennore, Chittagong, Colombo, Kolkata-Haldia, Mongla, Paradip, Port Blair, Matarbari, Thoothukudi, Visakhapatnam and Dhamra. Among the smaller ports are Gopalpur Port, Kakinada and Payra.
Background[edit | edit source]
Extent[edit | edit source]
- On the east: A line running from Cape Negrais (16°03'N) in Burma through the larger islands of the Andaman group, in such a way that all the narrow waters between the islands lie Eastward of the line and are excluded from the Bay of Bengal, as far as a point in Little Andaman Island in latitude 10°48'N, longitude 92°24'E and thence along the Southwest limit of the Burma Sea [A line running from "Oedjong Raja" ["Ujung Raja" or "Point Raja"] ( ) in Sumatra to Poeloe Bras (Breuëh) and on through the Western Islands of the Nicobar Group to Sandy Point in Little Andaman Island, in such a way that all the narrow waters appertain to the Burma Sea].
Etymology[edit | edit source]
The bay gets its name from the historical Bengal region (Modern-day Bangladesh and the Indian state of West Bengal). In ancient scriptures, this water body may have been referred to as 'Mahodadhi' (Sanskrit: महोदधि, lit. great water receptacle)[better source needed] while it appears as Sinus Gangeticus or Gangeticus Sinus, meaning "Gulf of the Ganges", in ancient maps.
The other Sanskrit name for Bay of Bengal is 'Purvapayodhi' (Sanskrit: पूर्वपयोधि, lit. Eastern Ocean).
History[edit | edit source]
In ancient Classical India, the Bay of Bengal was known as Kalinga Sagar (Kalinga Sea). Northern Circars occupied the western coast of the Bay of Bengal and is now considered to be India's Odisha and Andhra Pradesh state. Chola dynasty (9th century to 12th century) when ruled by Rajaraja Chola I and Rajendra Chola I occupied and controlled the Bay of Bengal with Chola Navy circa AD 1014, The Bay of Bengal was also called the Chola Sea or Chola Lake. The Kakatiya dynasty reached the western coastline of the Bay of Bengal between the Godavari and the Krishna rivers. Kushanas about the middle of the 1st century AD invaded northern India perhaps extending as far as the Bay of Bengal. Chandragupta Maurya extended the Maurya Dynasty across northern India to the Bay of Bengal. Hajipur was a stronghold for Portuguese Pirates. In the 16th century the Portuguese built trading posts in the north of the Bay of Bengal at Chittagong (Porto Grande) and Satgaon (Porto Pequeno).
Historic sites[edit | edit source]
In alphabetical order:
- Antarvedi is a popular place of worship Southern India, in East Godavari district of Andhra Pradesh devoted to Sri Lakshmi Narasimha Swamy Temple. This is the place where one of the distributaries of Godavari River meets the Bay of Bengal.
- Arikamedu is an archaeological site in Southern India, in Kakkayanthope, Ariyankuppam Commune, Puducherry. It is 4 kilometres (2.5 mi) from the capital, Pondicherry of the Indian territory of Puducherry
- British penal colony: Cellular Jail or "Black Waters" built in 1896 on Ross Island, a part of the Andaman Island Chain. As early as 1858 this island was used as a British penal colony for political prisoners facing life imprisonment.[better source needed]
- Buddhist heritage sites of Pavurallakonda, Thotlakonda and Bavikonda lie along the coast of Bay of Bengal at Visakhapatnam in India.
- Konark is the home of the Sun Temple or Black Pagoda. This Brahman sanctuary was built of black granite mid-1200 AD and has been declared a World Heritage Site.
- Jagannath Temple at Puri is the one of the four sacred places in Hindu pilgrimage along with Puri beach on the banks of Bay of Bengal. Mahodadhi was named after Lord Jagannath.
- Ramanathaswamy Temple is at Dhanushkodi, where the Bay of Bengal and the Gulf of Mannar come together.
- Seven Pagodas of Mahabalipuram is the name for Mahabalipuram. Mahabalipuram's Shore Temple, a World Heritage Site was constructed in the 8th century AD and myth has it that six other temples were built here.
- Sri Vaisakheswara Swamy temple lie under the Bay of Bengal. Spokespeople from Andhra University Centre for Marine Archaeology say the temple may be opposite the Coastal Battery.
- Vivekanandar Illam: It was constructed in 1842 by the American "Ice King" Frederic Tudor to store and market ice year round. In 1897, Swami Vivekananda's famous lectures were recorded here at Castle Kernan. The site is an exhibition devoted to Swami Vivekananda and his legacy.
Marine archaeology[edit | edit source]
Maritime archaeology or marine archaeology is the study of how ancient peoples interacted with the sea and waterways. A specialized branch, archaeology of shipwrecks, studies the salvaged artifacts of ancient ships. Stone anchors, amphorae shards, elephant tusks, hippopotamus teeth, ceramic pottery, a rare wood mast and lead ingots are examples which may survive submerged for centuries for archaeologists to discover, study, and place their salvaged findings into the timeline of history. Coral reefs, tsunamis, cyclones, mangrove swamps, battles, and a criss-cross of sea routes in a high trading area combined with piracy have all contributed to shipwrecks in the Bay of Bengal.
Shipwrecks and important shipping incidences[edit | edit source]
In chronological order:
- 1778 to 1783: The Naval operations in the American Revolutionary War or American War of Independence ranged as far as the Bay of Bengal.
- c. 1816: Mornington ship burned in the Bay of Bengal.
- 1850: American clipper brig Eagle is supposed to have sunk in the Bay of Bengal.
- American Baptist missionary Adoniram Judson died 12 April 1850 and was buried at sea in the Bay of Bengal.
- 1855: The Bark "Incredible" struck on a sunken rock in the Bay of Bengal.
- 1865: a gale dismasted the Euterpe while traversing the Bay of Bengal typhoon.
- 1875: Veleda - 76 m (250 ft) long and 15 m (50 ft) wide. It is part of a current salvage operation.
- 1942: Japanese cruiser Yura of the Second Expeditionary Fleet, Malay Force, attacked merchant ships in the Bay of Bengal.
- 1971: December 3 – Pakistan Navy submarine PNS Ghazi sunk under mysterious circumstances, near Visakhapatnam, in the Bay of Bengal.
Significance[edit | edit source]
Economic importance[edit | edit source]
One of the first trading ventures along the Bay of Bengal was The Company of Merchants of London Trading into the East Indies, more commonly referred to as the British East India Company. Gopalpur-on-Sea was one of their main trading centers. Other trading companies along the Bay of Bengal shorelines were the English East India Company and the French East India Company.
BIMSTEC (Bay of Bengal Initiative for Multi-Sectoral Technical and Economic Cooperation) supports free trade internationally around the Bay of Bengal between Bangladesh, Bhutan, India, Myanmar, Nepal, Sri Lanka, and Thailand.
The Sethusamudram Shipping Canal Project is a new venture proposed which would create a channel for a shipping route to link the Gulf of Mannar with the Bay of Bengal. This would connect India from east to west without the necessity of going around Sri Lanka.
Thoni and catamaran fishing boats of fishing villages thrive along the Bay of Bengal shorelines. Fishermen can catch between 26 and 44 species of marine fish. In one year, the average catch is two million tons of fish from the Bay of Bengal alone. Approximately 31% of the world's coastal fishermen live and work on the bay.
Geostrategic importance[edit | edit source]
The Bay of Bengal is centrally located in South and Southeast Asia. It lies at the center of two huge economic blocks, the SAARC and ASEAN. It influences China's southern landlocked region in the north and major sea ports of India and Bangladesh. China, India, and Bangladesh have forged naval cooperation agreements with Malaysia, Thailand and Indonesia to increase cooperation in checking terrorism in the high seas.
Its outlying islands (the Andaman and Nicobar Islands) and, most importantly, major ports such as Paradip Kolkata, Chennai, Visakhapatnam, Tuticorin, Chittagong, and Mongla, along its coast with the Bay of Bengal added to its importance.
China has recently made efforts to project influence into the region through tie-ups with Myanmar and Bangladesh. The United States has held major exercises with Bangladesh, Malaysia, Singapore, Thailand and recently India. The largest ever wargame in Bay of Bengal, known as Malabar 2007, was held in 2007 and naval warships from US, Bangladesh, Thailand, Singapore, Japan and Australia took part. India was a participant.
Large deposits of natural gas in the areas within Bangladesh's sea zone incited a serious urgency by India and Myanmar into a territorial dispute. Disputes over rights of some oil and gas blocks have caused brief diplomatic spats between Myanmar and India with Bangladesh.
The disputed maritime boundary between Bangladesh and Myanmar resulted in military tensions in 2008 and 2009. Bangladesh is pursuing a settlement with Myanmar and India to the boundary dispute through the International Tribunal on the Law of the Sea.
Religious importance[edit | edit source]
The Samudra arati is a daily tradition started by the present Shankaracharya of Puri 9 years ago to honour the sacred sea. The daily practise includes prayer and fire offering to the sea at Swargadwar in Puri by disciples of the Govardhana matha of the Shankaracharya. On Paush Purnima of every year the Shankaracharya himself comes out to offer prayers to the sea.
Key features[edit | edit source]
Beaches[edit | edit source]
Islands[edit | edit source]
The islands in the bay are numerous, including the Andaman Islands, Nicobar Islands and Mergui Archipelago of India and Myanmar. The Cheduba group of islands, in the north-east, off the Burmese coast, are remarkable for a chain of mud volcanoes, which are occasionally active.
Great Andaman is the main archipelago or island group of the Andaman Islands, whereas Ritchie's Archipelago consists of smaller islands. Only 37, or 6.5%, of the 572 islands and islets of the Andaman and Nicobar Islands are inhabited.
Rivers[edit | edit source]
Many major Rivers of India and Bangladesh flow west to east before draining into the Bay of Bengal. The Ganga is the northernmost of these rivers. Its main channel enters and flows through Bangladesh, where it is known as the Padma River, before joining the Meghna River. However, the Brahmaputra River flows from east to west in Assam before turning south and entering Bangladesh where it is called the Jamuna River. This joins the Padma where upon the Padma joins the Meghna River that finally drains into Bay of Bengal. The Sundarbans is a mangrove forest in the southern part of the Ganges-Brahmaputra Delta which lies in the Indian state of West Bengal and in Bangladesh. The Brahmaputra at 2,948 km (1,832 mi) is the 28th longest River in the world. It originates in Tibet. The Hooghly River, another channel of the Ganga that flows through Kolkata drains into Bay of Bengal at Sagar in West Bengal, India.
The Ganga–Brahmaputra-Barak rivers deposit nearly 1000 million tons of sediment every year. The sediment from these three rivers form the Bengal Delta and the submarine fan, a vast structure that extends from Bengal to south of the Equator, is up to 16.5 kilometres (10.3 mi) thick, and contains at least 1,130 trillion tonnes of sediment, which has accumulated over the last 17 million years at an average rate of 665 million tons per annum. The fan has buried organic carbon at a rate of nearly 1.1 trillion mol/yr (13.2 million t/yr) since the early Miocene period. The three rivers currently contribute nearly 8% of the total organic carbon (TOC) deposited in the world's oceans. Due to high TOC accumulation in the deep sea bed of the Bay of Bengal, the area is rich in oil and natural gas and gas hydrate reserves. Bangladesh can reclaim land substantially and economically gain from the sea area by constructing sea dikes, bunds, causeways and by trapping the sediment from its rivers.
Further southwest of Bengal, the Mahanadi, Godavari, Krishna and Kaveri Rivers also flow from west to east across Deccan Plateau in Peninsular India and drain into the Bay of Bengal forming deltas. Many small rivers also drain directly into the Bay of Bengal forming estuaries; the shortest of them is the Cooum River at 64 km (40 mi).
Seaports[edit | edit source]
Indian ports on the bay include Paradip Port, Kolkata Port, Haldia Port, Chennai, Visakhapatnam, Kakinada, Pondicherry, Dhamra, Gopalpur and Bangladeshi ports on the Bay are Chittagong, Mongla, Payra Port.
Oceanography[edit | edit source]
In alphabetical order.
Geology[edit | edit source]
Lithosphere and plate tectonics[edit | edit source]
The lithosphere of the earth is broken up into what are called tectonic plates. Underneath the Bay of Bengal, which is part of the great Indo-Australian Plate and is slowly moving north east. This plate meets the Burma Microplate at the Sunda Trench. The Nicobar Islands and the Andaman Islands are part of the Burma Microplate. The India Plate subducts beneath the Burma Plate at the Sunda Trench or Java Trench. Here, the pressure of the two plates on each other increase pressure and temperature resulting in the formation of volcanoes such as the volcanoes in Myanmar, and a volcanic arc called the Sunda Arc. The Sumatra-Andaman earthquake and Asian tsunami was a result of the pressure at this zone causing a submarine earthquake which then resulted in a destructive tsunami.
Marine geology[edit | edit source]
A zone 50 m wide extending from the island of Sri Lanka and the Coromandel coast to the head of the bay, and thence southwards through a strip embracing the Andaman and Nicobar islands, is bounded by the 100 fathom line of sea bottom; some 50 m. beyond this lies the 500-fathom limit. Opposite the mouth of the Ganges, however, the intervals between these depths are very much extended by deltaic influence.
Swatch of No Ground is a 14 km-wide deep sea canyon of the Bay of Bengal. The deepest recorded area of this valley is about 1340 m. The submarine canyon is part of the Bengal Fan, the largest submarine fan in the world.
Submarine fans[edit | edit source]
Submarine fan is also known as abyssal fan. Bay of Bengal fan, known as Bengal Fan, also known as the Ganges Fan is world's largest abyssal fan, also known as deep-sea fans, underwater deltas, and submarine fans. The fan is about 3,000 km (1,900 mi) long, 1,430 km (890 mi) wide with a maximum thickness of 16.5 km (10.3 mi). The fan resulted from the uplift and erosion of the Himalayas and the Tibetan Plateau produced by the collision between the Indian Plate and the Eurasian Plate. Most of the sediment is supplied by the Ganges and Brahmaputra rivers which supply the Lower Meghna delta in Bangladesh and the Hoogly delta in West Bengal (India). Several other large rivers in Bangladesh and India provide smaller contributions. Turbidity currents have transported the sediment through a series of submarine canyons, some of which are more than 2,400 kilometres (1,500 mi) in length, to be deposited in the Bay of Bengal up to 30 degrees latitude from where it began. To date, the oldest sediments recovered from the Bengal fan are from Early Miocene age. Their mineralogical and geochemical characteristics allow to identify their Himalayan origin and demonstrate that the Himalaya was already a major mountain range 20 million years ago.
The fan completely covers the floor of the Bay of Bengal. It is bordered to the west by the continental slope of eastern India, to the north by the continental slope of Bangladesh and to east by the northern part of Sunda Trench off Myanmar and the Andaman Islands, the accretionary wedge associated with subduction of the Indo-Australian Plate beneath the Sunda Plate and continues along the west side of the Ninety East Ridge. The Nicobar Fan, another lobe of the fan, lies east of the Ninety East Ridge.
The fan was first identified by bathymetric survey in the sixties by Bruce C. Heezen and Marie Tharp which identified the abyssal cone and canyon structures. It was delineated and named by Joseph Curray and David Moore following a geological and geophysical survey in 1968.
Oceanographic chemistry[edit | edit source]
Coastal regions bordering the Bay of Bengal are rich in minerals. Sri Lanka, Serendib, or Ratna – Dweepa which means Gem Island. Amethyst, beryl, ruby, sapphire, topaz, and garnet are just some of the gems of Sri Lanka. Garnet and other precious gems are also found in abundance in the Indian states of Odisha and Andhra Pradesh.
Oceanographic climate[edit | edit source]
From January to October, the current is northward flowing, and the clockwise circulation pattern is called the "East Indian Current". The Bay of Bengal monsoon moves in a northwest direction striking the Nicobar Islands, and the Andaman Islands first end of May, then coast of Mainland India by end of June.
The remainder of the year, the counterclockwise current is southwestward flowing, and the circulation pattern is called the East Indian Winter Jet. September and December see very active weather, season varsha (or monsoon), in the Bay of Bengal producing severe cyclones which affect eastern India. Several efforts have been initiated to cope with storm surge.
Marine biology, flora and fauna[edit | edit source]
The Bay of Bengal is full of biological diversity, diverging amongst coral reefs, estuaries, fish spawning and nursery areas, and mangroves. The Bay of Bengal is one of the World's 64 largest marine ecosystems.
Kerilia jerdonii is a sea snake of the Bay of Bengal. Glory of Bengal cone (Conus bengalensis) is just one of the seashells which can be photographed along beaches of the Bay of Bengal. An endangered species, the olive ridley sea turtle can survive because of the nesting grounds made available at the Gahirmatha Marine Wildlife Sanctuary, Gahirmatha Beach, Odisha, India. Marlin, barracuda, skipjack tuna, (Katsuwonus pelamis), yellowfin tuna, Indo-Pacific humpbacked dolphin (Sousa chinensis), and Bryde's whale (Balaenoptera edeni) are a few of the marine animals. Bay of Bengal hogfish (Bodianus neilli) is a type of wrasse which live in turbid lagoon reefs or shallow coastal reefs. Schools of dolphins can be seen, whether they are the bottle nose dolphin (Tursiops truncatus), pantropical spotted dolphin (Stenella attenuata) or the spinner dolphin (Stenella longirostris). Tuna and dolphins usually reside in the same waters. In shallower and warmer coastal waters the Irrawaddy dolphins (Orcaella brevirostris) can be found.
The Great Nicobar Biosphere Reserve provides sanctuary to many animals some of which include the saltwater crocodile (Crocodylus porosus), giant leatherback sea turtle (Dermochelys coriacea), and Malayan box turtle (Cuora amboinensis kamaroma) to name a few.
Transboundary issues[edit | edit source]
A transboundary issue is defined as an environmental problem in which either the cause of the problem and/or its impact is separated by a national boundary; or the problem contributes to a global environmental problem and finding regional solutions is considered to be a global environmental benefit. The eight Bay of Bengal countries have (2012) identified three major transboundary problems (or areas of concern) affecting the health of the Bay, that they can work on together. With the support of the Bay Of Bengal Large Marine Ecosystem Project (BOBLME), the eight countries are now (2012) developing responses to these issues and their causes, for future implementation as the Strategic Action Programme.
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Ecological degradation[edit | edit source]
Fisheries overexploitation[edit | edit source]
Fisheries production in the Bay of Bengal is six million tonnes per year, more than seven percent of the world's catch. The major transboundary issues relating to shared fisheries are: a decline in the overall availability of fish resources; changes in species composition of catches; the high proportion of juvenile fish in the catch; and changes in marine biodiversity, especially through loss of vulnerable and endangered species. The transboundary nature of these issues are: that many fish stocks are shared between BOBLME countries through the transboundary migration of fish, or larvae. Fishing overlaps national jurisdictions, both legally and illegally – overcapacity and overfishing in one location forces a migration of fishers and vessels to other locations. All countries (to a greater or lesser degree) are experiencing difficulties in implementing fisheries management, especially the ecosystem approach to fisheries. Bay of Bengal countries contribute significantly to the global problem of loss of vulnerable and endangered species. The main causes of the issues are: open access to fishing grounds; Government emphasis on increasing fish catches; inappropriate government subsidies provided to fishers; increasing fishing effort, especially from trawlers and purse seiners; high consumer demand for fish, including for seed and fishmeal for aquaculture; ineffective fisheries management; and illegal and destructive fishing.
Marine habitats degradation[edit | edit source]
The Bay of Bengal is an area of high biodiversity, with many endangered and vulnerable species. The major transboundary issues relating to habitats are: the loss and degradation of mangrove habitats; degradation of coral reefs; and the loss of, and damage to, seagrasses. The transboundary nature of these major issues are: that all three critical habitats occur in all BOBLME countries. Coastal development for several varying uses of the land and sea are common in all BOBLME countries. Trade in products from all the habitats is transboundary in nature. Climate change impacts are shared by all BOBLME countries. The main causes of the issues are: food security needs of the coastal poor; lack of coastal development plans; increasing trade in products from coastal habitats; coastal development and industrialization; ineffective marine protected areas and lack of enforcement; upstream development that affects water-flow; intensive upstream agricultural practices; and increasing tourism.
Environmental degradation[edit | edit source]
Environmental hazards[edit | edit source]
The Asian brown cloud, a layer of air pollution that covers much of South Asia and the Indian Ocean every year between January and March, and possibly also during earlier and later months, hangs over the Bay of Bengal. It is considered to be a combination of vehicle exhaust, smoke from cooking fires, and industrial discharges. Because of this cloud, satellites attempting to track ocean acidification and other ocean health indicators in the Bay have difficulty obtaining accurate measurements.
Pollution and water quality[edit | edit source]
The major transboundary issues relating to pollution and water quality are: sewage-borne pathogens and organic load; solid waste/marine litter; increasing nutrient inputs; oil pollution; persistent organic pollutants (POPs) and persistent toxic substances (PTSs); sedimentation; and heavy metals. The transboundary nature of these issues are: discharge of untreated/partially treated sewage being a common problem. Sewage and organic discharges from the Ganges-Brahmaputra-Meghna River are likely to be transboundary. Plastics and derelict fishing gear can be transported long distances across national boundaries. High nutrient discharges from rivers could intensify largescale hypoxia. Atmospheric transport of nutrients is inherently transboundary. Differences between countries with regard to regulation and enforcement of shipping discharges may drive discharges across boundaries. Tar balls are transported long distances. POPs/PTSs and mercury, including organo-mercury, undergo long-range transport. Sedimentation and most heavy metal contamination tend to be localized and lack a strong transboundary dimension. The main causes of the issues are: increasing coastal population density and urbanization; higher consumption, resulting in more waste generated per person; insufficient funds allocated to waste management; migration of industry into BOBLME countries; and proliferation of small industries.
Tropical storms and cyclones[edit | edit source]
A tropical storm with rotating winds blowing at speeds of 119 km/h (74 mph) is called a cyclone when they originate over the Bay of Bengal, and called a hurricane in the Atlantic. Between 100,000 and 500,000 residents of Bangladesh were killed because of the 1970 Bhola cyclone.
- 2021, Very Severe Cyclonic Storm Yaas
- 2020, Very Severe Cyclonic Storm Nivar
- 2020, Super Cyclonic Storm Amphan
- 2019, Very Severe Cyclonic Storm Bulbul
- 2019, Extremely Severe Cyclonic Storm Fani
- 2018, Very Severe Cyclonic Storm Gaja
- 2018, Cyclone Titli
- 2017, Severe Cyclonic Storm Mora
- 2017, Cyclone Maarutha
- 2016, Very Severe Cyclonic Storm Vardah
- 2016, Cyclone Nada
- 2016, Cyclone Kyant
- 2016, Cyclone Roanu
- 2015, Cyclone Komen
- 2014, Very Severe Cyclonic Storm Hudhud
- 2013, Very Severe Cyclonic Storm Phailin
- 2013, Cyclone Viyaru
- 2012, Cyclone Nilam
- 2011, Very Severe Cyclonic Storm Thane
- 2010, Very Severe Cyclonic Storm Giri
- 2009, Very Severe Cyclonic Storm Aila
- 2008, Very Severe Cyclonic Storm Nargis
- 2007, Very Severe Cyclonic Storm Sidr
- 2006, Very Severe Cyclonic Storm Mala
- 1999, Odisha Super Cyclonic Storm 05B
- 1996, Konaseema Cyclone
- 1991, Super Cyclonic Storm 02B
- 1989, November Typhoon Gay
- 1985, May Tropical Storm One (1B)
- 1982, April Cyclone One (1B)
- 1982, May Tropical Storm Two (2B)
- 1982, October Tropical Storm Three (3B)
- 1981, December Cyclone Three (3B)
- 1980, October Tropical Storm One (1B)
- 1980, December Unknown Storm Four (4B)
- 1980, December Tropical Storm Five (5B)
- 1977, Andhra Pradesh Cyclone (6B)
- 1971, Odisha cyclone
- 1970, November Bhola cyclone
- The 1864 Calcutta Cyclone: caused a storm surge of 40 feet. Barometer 28.025 inches of mercury. 50,000 direct deaths and 30,000 from disease.
- The Backergunge cyclone of 1876: 10 to 30 or 40 feet storm surge. 100,000 direct deaths and 100,000 indirect from disease.
- The False Point cyclone of 1885: 22 feet of storm surge. Barometer 27.135 inches of mercury.
See also[edit | edit source]
References[edit | edit source]
- "Map of Bay of Benglal- World Seas, Bay of Bengal Map Location – World Atlas". 4 February 2021.
- Chowdhury, Sifatul Quader (2012). "Bay of Bengal". In Islam, Sirajul; Jamal, Ahmed A. (eds.). Banglapedia: National Encyclopedia of Bangladesh (Second ed.). Asiatic Society of Bangladesh.
- "Limits of Oceans and Seas, 3rd edition" (PDF). International Hydrographic Organization. 1953. Archived from the original (PDF) on 8 October 2011. Retrieved 28 December 2020.
- Glossary of Terms Appearing on Maps of the Netherlands East Indies, United States Army Map Service, page 115.
- Kuttan (2009). The Great Philosophers of India. AuthorHouse. ISBN 978-1434377807.[self-published source]
- "Dhanushkodi". indiatourism4u.in. Archived from the original on 8 March 2014. Retrieved 21 August 2013.
- 1794, Orbis Veteribus Notus by Jean Baptiste Bourguignon d'Anville
- Agarwala, Nitin (2020), "The Re-Emergence of the Bay of Bengal", The Journal of Territorial and Maritime Studies, McFarland & Company, 7 (2): 52
- Mohanty, PC (November 2011), Maritime Trade of Ancient Kalinga (PDF), Orissa Review, p. 41
- The Portuguese in Bengal. History of Ugolim (Hoogli), Meliapore ... Archived 3 February 2007 at the Wayback Machine URL accessed 21 January 2007
- Chakravorty, Sohini (5 January 2012). "In the lap of Godavari, all the time to sit and stare". The Hindu.
- "History of Andaman Cellular Jail: Recapture of Andaman Islands to keep Political Prisoners". AndamanCellularJail.org. Archived from the original on 13 January 2007. Retrieved 6 August 2010.
- "Ramayana". Ramayana.com. 16 August 2005. Archived from the original on 16 August 2005.
- Morien Institute – underwater discoveries news archive, January–June 2006, "Sri Vaisakheswara still lies underwater" URL accessed 22 January 2007
- Marine Archaeology in India URL accessed 22 January 2007
- Shipwrecks 1816–1818 URL accessed 10 January 2015
- The Maritime Heritage Project: Gold Rush Ships, Passengers, Captains URL accessed 23 January 2007
- Shipping Notes from the 1800s – P.E.I. URL accessed 23 January 2007
- Diving-News.com » Wrecks URL accessed 23 January 2007
- Nabataea: Trade on the Bay of Bengal URL accessed 21 January 2007
- "Environmental assessment of coastal water at Bakkhali" (PDF). Archived from the original (PDF) on 26 February 2015.
- "LME 34 Bay of Bengal". NOAA. Archived from the original on 18 April 2003. Retrieved 21 January 2007.
- "The Bay of Bengal: New bay dawning". The Economist. 27 April 2013.
- Berlin, Donald L. (25 January 2005). "The emerging Bay of Bengal". Asia Times Online. Archived from the original on 29 January 2005.CS1 maint: unfit URL (link)
- Arpi, Claude (26 December 2006). "1971 War: How the US tried to corner India". Rediff.com.
- "The Burma Project -Burma Debate". Archived from the original on 18 September 2009. Retrieved 10 January 2015.
- "India's Largest Naval War Game in Bay of Bengal". Global Politician. Archived from the original on 15 October 2012.
- Parameswaran, Prashanth (7 May 2015). "US Eyes Expanded Military Exercises with ASEAN Navies". The Diplomat. Retrieved 11 November 2015.
- Miglani, Sanjeev (22 July 2015). "India, Japan, U.S. plan naval exercises in tightening of ties in Indian Ocean". Reuters. Archived from the original on 4 December 2015. Retrieved 11 November 2015.
- Gady, Franz-Stefan (13 October 2015). "Confirmed: Japan Will Permanently Join US-India Naval Exercises". The Diplomat. Retrieved 11 November 2015.
- "The Maritime Boundary Dispute Between Bangladesh and Myanmar: Motivations, Potential Solutions, and Implications".
- Sahu, Monideepa (6 March 2016). "The great fire". Deccan Herald. Retrieved 6 March 2016.
- Siddiqui, Neaz Ahmad (2012). "Sundarbans, The". In Islam, Sirajul; Jamal, Ahmed A. (eds.). Banglapedia: National Encyclopedia of Bangladesh (Second ed.). Asiatic Society of Bangladesh.
- "World's longest beach hidden in Bangladesh". The Sydney Morning Herald. 31 January 2007.
- One or more of the preceding sentences incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Bengal, Bay of". Encyclopædia Britannica (11th ed.). Cambridge University Press.
- The long stretch of sand glistening like silver dust URL accessed 10 January 2015
- Wasson, Robert (2003). "A sediment budget for the Padma-Meghna-Jamuna catchment" (PDF). Current Science. 84 (8): 1041–1047.
- Tsunami Archived 27 September 2007 at the Wayback Machine URL access 21 January 2007
- Morphological features in the Bay of Bengal Archived 14 June 2007 at the Wayback Machine URL accessed 21 January 2007
- Curray, Joseph R.; Frans J. Emmel; David G. Moore (December 2002). "The Bengal Fan: morphology, geometry, stratigraphy, history and processes". Marine and Petroleum Geology. Elsevier Science Ltd. 19 (10): 1191–1223. doi:10.1016/S0264-8172(03)00035-7.
- France-Lanord, Christian; Volkhard Spiess; Peter Molnar; Joseph R. Curray (March 2000). "Summary on the Bengal Fan: An introduction to a drilling proposal" (PDF). Woods Hole Oceanographic Institution. Archived from the original (PDF) on 5 October 2011. Retrieved 16 September 2011.
- Shanmugam, G. (2016). "Submarine fans: A critical retrospective (1950–2015)". Journal of Palaeogeography. 5 (2): 110–184. Bibcode:2016JPalG...5..110S. doi:10.1016/j.jop.2015.08.011.
- Cochran, J.R.; Stow, D.A.V.; et al. (1989). Cochran, J.R; Stow, D.A.V (eds.). "116 Initial Reports Table of Contents". Proc. ODP, Init. Repts. Proceedings of the Ocean Drilling Program. Ocean Drilling Program College Station, TX. 116. doi:10.2973/odp.proc.ir.116.1989.
- France-Lanord, Christian; Derry L.; Michard A. (1993). "Evolution of the Himalaya since Miocene time: isotopic and sedimentological evidence from the Bengal Fan" (PDF). Geological Society Special Publication. 74 (1): 603–621. Bibcode:1993GSLSP..74..603F. doi:10.1144/GSL.SP.1993.074.01.40. S2CID 85506590.
- Tilmann Schwenk; Volkhard Spiess (2009). "Architecture and Stratigraphy of the Bengal Fan as Response to Tectonic and Climate Revealed from High-Resolution Seismic Data". SEPM Special Publication, No. 92. External Controls on Deep-Water Depositional Systems. SEPM (Society for Sedimentary Geology). pp. 107–131. ISBN 978-1-56576-136-0.
- Curray, Joseph R.; David G. Moore (March 1971). "Growth of the Bengal Deep-Sea Fan and Denudation in the Himalayas". Geological Society of America Bulletin. 82 (3): 563–572. Bibcode:1971GSAB...82..563C. doi:10.1130/0016-7606(1971)82[563:GOTBDF]2.0.CO;2.
- "Promise Rings in white gold, yellow gold, rose gold, unique rings. by A Ring Thing".
- Glossary of Physical Oceanography Ba-Bm Archived 18 October 2007 at the Wayback Machine URL accessed 21 January 2007
- Phillip Colla Natural History Photography URL accessed 21 January 2007
- Haider, Mashida R. (5 January 2005). "Naturalist". New Age. Dhaka. Archived from the original on 30 November 2010.
- CMS: Stenella attenuata, Pantropical spotted dolphin Archived 3 February 2007 at the Wayback Machine URL accessed 21 January 2007
- 17 Bay of Bengal URL accessed 21 January 2007
- "Bodianus neilli (Bay of Bengal Hogfish)". Zipcode Zoo. Archived from the original on 30 May 2008. Retrieved 21 January 2007.
- "EO Natural Hazards: Smog over the Bay of Bengal". NASA Earth Observatory. Archived from the original on 26 October 2007. Retrieved 21 January 2007.
- Ocean acidification in Bay of Bengal is now being monitored Firstpost, 16 December 2019.
- "Forces of Nature—Natural Disaster Fast Facts". National Geographic. Retrieved 30 August 2016.
- Tannehill, Ivan Ray (1969) [First published 1945]. Hurricanes: Their Nature and History: Particularly Those of the West Indies and the Southern Coasts of the United States (6th ed.). Princeton University Press. pp. 38–40. ISBN 9780837123165.
Further reading[edit | edit source]
- The Maritime Boundary Dispute Between Bangladesh and Myanmar: Motivations, Potential Solutions, and Implications by Jared Bissinger (Asia Policy, July 2010) published by National Bureau of Asian Research
[edit | edit source]
- 487 V. Suryanarayan, Prospects for a Bay of Bengal Community
- Arabian Sea: depth contours and undersea features – Map/Still – Britannica Concise
- Bay of Bengal in Encyclopedia
- Bay of Bengal Large Marine Ecosystem Project