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Kawthoung District In Tanintharyi Region
Kawthaung ( mnw, ကော့ပိ, , ; th, เกาะสอง; , ; ms, Pulodua, ڤولودوا) is a town located in the southernmost part of Myanmar, in the Tanintharyi Region. During British rule in Burma between 1824 and 1948, it was known as Victoria Point. As of 2021, it has a population of 57,949. History Rakhine and Tanintharyi were transferred to British rule after the First Anglo-Burmese War of 1823–1826. In 1859, a local group of Chinese and Thais settled at Maliwan (Thai language) to the north of Kawthaung, a place with numerous lakes and flowering trees. In 1865, an Arab–Malay group led by Nayuda Ahmed, traveling and collecting sea products around Mergui Archipelago started a base and village at the bay of Victoria Point. In 1872 the third mayor of Mergui District, Sir Ashly Din (1870–1875) assigned the first police officer to be stationed at Maliwan, a village 24 miles north of current Victoria Point. In 1891, the local government offices were moved ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Administrative Divisions Of Burma
Myanmar is divided into twenty-one administrative subdivisions, which include 7 regions, 7 states, 1 union territory, 1 self-administered division, and 5 self-administered zones. Following is the table of government subdivisions and its organizational structure based on different regions, states, the union territory, the self-administered division, and the self-administered zones: The regions were called divisions prior to August 2010, and four of them are named after their capital city, the exceptions being Sagaing Region, Ayeyarwady Region and Tanintharyi Region. The regions can be described as ethnically predominantly Burman (Bamar), while the states, the zones and Wa Division are dominated by ethnic minorities. Yangon Region has the largest population and is the most densely populated. The smallest population is Kayah State. In terms of land area, Shan State is the largest and Naypyidaw Union Territory is the smallest. Regions and states are divided into districts ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ranong
Ranong ( th, ระนองPronunciation) is a town (''thesaban mueang'') in southern Thailand, capital of the Ranong Province and the Mueang Ranong District. The town covers completely the area of the ''tambon'' Khao Niwet (เขานิเวศน์). As of 2005, it had a population of 16,163. Ranong lies south-southwest of Bangkok by road. Geography Ranong is on the estuary of the Pak Chan (or Kraburi) River, opposite Myanmar's Kawthaung (formerly Victoria Point). The Tenasserim Hills rise directly to the east of Ranong, and another small ridge runs along the edge of the estuary to the town's north. Climate Ranong has a tropical monsoon climate (Köppen climate classification ''Am''). There is little variation in the temperature throughout the year, although the pre-monsoon months (February to April) are somewhat hotter in the day. However, Ranong's position to the west of the Tenasserim Hills means that the monsoon season's rains are greatly amplified, resulting in to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mon People
The Mon ( mnw, ဂကူမည်; my, မွန်လူမျိုး, ; th, มอญ, ) are an ethnic group who inhabit Lower Myanmar's Mon State, Kayin State, Kayah State, Tanintharyi Region, Bago Region, the Irrawaddy Delta, and several areas in Thailand (mostly in Pathum Thani province, Phra Pradaeng and Nong Ya Plong). There are also small numbers of Mon people in West Garo Hills, calling themselves Man or Mann, who also came from Myanmar to Assam, ultimately residing in Garo Hills. The native language is Mon, which belongs to the Monic branch of the Mon-Khmer language family and shares a common origin with the Nyah Kur language, which is spoken by the people of the same name that live in Northeastern Thailand. A number of languages in Mainland Southeast Asia are influenced by the Mon language, which is also in turn influenced by those languages. The Mon were one of the earliest to reside in Southeast Asia, and were responsible for the spread of Theravada Bu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karen People
The Karen, kjp, ပ်ုဖၠုံဆိုဒ်, my, ကရင်လူမျိုး, , th, กะเหรี่ยง ( ), also known as the Kayin, Kariang or Kawthoolese, are an ethnolinguistic group of Sino-Tibetan language–speaking peoples. The group as a whole is heterogeneous and disparate as many Karen ethnic groups do not associate or identify with each other culturally or linguistically. These Karen groups reside primarily in Kayin State, southern and southeastern Myanmar. The Karen, approximately five million people, account for approximately seven percent of the Burmese population. Many Karen have migrated to Thailand, having settled mostly on the Myanmar–Thailand border. A few Karen have settled in the Andaman and Nicobar Islands, India, and other Southeast Asian and East Asian countries. The Karen groups as a whole are often confused with the Padaung tribe, best known for the neck rings worn by their women, but t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shan People
The Shan people ( shn, တႆး; , my, ရှမ်းလူမျိုး; ), also known as the Tai Long, or Tai Yai are a Tai ethnic group of Southeast Asia. The Shan are the biggest minority of Burma (Myanmar) and primarily live in the Shan State of this country, but also inhabit parts of Mandalay Region, Kachin State, and Kayin State, and in adjacent regions of China ( Dai people), Laos, Assam (Ahom people) and Thailand. Though no reliable census has been taken in Burma since 1935, the Shan are estimated to number 4–6 million, with CIA Factbook giving an estimate of five million spread throughout Myanmar which is about 10% of the overall Burmese population. 'Shan' is a generic term for all Tai-speaking peoples within Myanmar (Burma). The capital of Shan State is Taunggyi, the fifth-largest city in Myanmar with about 390,000 people. Other major cities include Thibaw (Hsipaw), Lashio, Kengtung and Tachileik. Etymology The Shan use the endonym Tai (တႆး) in r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thai People
Thai people ( th, ชาวไทย; ''endonym''), Central Thai people ( th, คนภาคกลาง, sou, คนใต้, ตามโพร; ''exonym and also domestically'') or Siamese ( th, ชาวสยาม; ''historical exonym and sometimes domestically''), T(h)ai Noi people ( th, ไทยน้อย; ''historical endonym and sometimes domestically''), in a narrow sense, are a Tai ethnic group dominant in Central and Southern Thailand (Siam proper). Part of the larger Tai ethno-linguistic group native to Southeast Asia as well as Southern China and Northeast India, Thais speak the Sukhothai languages ( Central Thai and Southern Thai language), which is classified as part of the Kra–Dai family of languages. The majority of Thais are followers of Theravada Buddhism. As a result of government policy during the 1930s and 1940s resulting in successful forced assimilation of many the various ethno-linguistic groups in the country into the dominant Thai language and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bamar
The Bamar (, ; also known as the Burmans) are a Sino-Tibetan ethnic group native to Myanmar (formerly Burma) in Southeast Asia. With approximately 35 million people, the Bamar make up the largest ethnic group in Myanmar, constituting 68% of the country's population. The geographic homeland of the Bamar is the Irrawaddy River basin. Burmese is the native language of the Bamar, as well as the national language and lingua franca of Myanmar. Ethnonyms In the Burmese language, Bamar (ဗမာ, also transcribed Bama) and Myanmar (မြန်မာ, also transliterated Mranma and transcribed Myanma) have historically been interchangeable endonyms. Burmese is a diglossic language; "Bamar" is the diglossic low form of "Myanmar," which is the diglossic high equivalent. The term "Myanmar" is extant to the early 1100s, first appearing on a stone inscription, where it was used as a cultural identifier, and has continued to be used in this manner. From the onset of British colonial r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deutscher Wetterdienst
The () or DWD for short, is the German Meteorological Service, based in Offenbach am Main, Germany, which monitors weather and meteorological conditions over Germany and provides weather services for the general public and for nautical, aviational, hydrometeorological or agricultural purposes. It is attached to the Federal Ministry for Digital and Transport. The DWDs principal tasks include warning against weather-related dangers and monitoring and rating climate changes affecting Germany. The organisation runs atmospheric models on their supercomputer for precise weather forecasting. The DWD also manages the national climate archive and one of the largest specialised libraries on weather and climate worldwide. History The DWD was formed in 1952 when the weather services of the western occupation zones were merged. In 1954, the Federal Republic of Germany joined the World Meteorological Organization (WMO). In 1990, following the reunification, the weather services of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World Meteorological Organization
The World Meteorological Organization (WMO) is a specialized agency of the United Nations responsible for promoting international cooperation on atmospheric science, climatology, hydrology and geophysics. The WMO originated from the International Meteorological Organization, a nongovernmental organization founded in 1873 as a forum for exchanging weather data and research. Proposals to reform the status and structure of the IMO culminated in the World Meteorological Convention of 1947, which formally established the World Meteorological Organization. The Convention entered into force on 23 March 1950, and the following year the WMO began operations as an intergovernmental organization within the UN system. The WMO is made up of 193 countries and territories, and facilitates the "free and unrestricted" exchange of data, information, and research between the respective meteorological and hydrological institutions of its members. It also collaborates with nongovernmental partners ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norwegian Meteorological Institute
The Norwegian Meteorological Institute ( no, Meteorologisk institutt), also known internationally as MET Norway, is Norway's national meteorological institute. It provides weather forecasts for civilian and military uses and conducts research in meteorology, oceanography and climatology. It is headquartered in Oslo and has offices and stations in other cities and places. It has around 500 full-time staff and was founded in 1866. History The institute was founded on 1 December 1866 with the help of Norwegian astronomer and meteorologist Henrik Mohn who served as its director until 1913. He is credited with founding meteorological research in Norway. The abbreviation ''MET Oslo'' or ''MET OSLO'' has been used internationally for a long time; the World Meteorological Organization for example recommended in 1956 that its members standardized references to this institute as ''MET OSLO''.Abridged Final Report of the Session, Commission for Marine Meteorology, Secretariat of the World ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropical Monsoon Climate
An area of tropical monsoon climate (occasionally known as a sub-equatorial, tropical wet climate or a tropical monsoon and trade-wind littoral climate) is a tropical climate sub-type that corresponds to the Köppen climate classification category ''Am''. Tropical monsoon climates have monthly mean temperatures above in every month of the year and a dry season. The tropical monsoon climate is the intermediate climate between the wet Af (or tropical rainforest climate) and the drier Aw (or tropical savanna climate). A tropical monsoon climate's driest month has on average less than 60 mm, but more than 100-\left(\frac\right). This is in direct contrast to a tropical savanna climate, whose driest month has less than 60 mm of precipitation and also less than 100-\left(\frac\right) of average monthly precipitation. In essence, a tropical monsoon climate tends to either have more rainfall than a tropical savanna climate or have less pronounced dry seasons. A tropical monsoon c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
