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111-812: The Tenasserim Hills or Tenasserim Range ( Burmese : တနင်္သာရီ တောင်တန်း , [tənɪ̀ɰ̃θàjì tàʊɰ̃dáɰ̃] ; Thai : ทิวเขาตะนาวศรี , RTGS :  Thio Khao Tanao Si , pronounced [tʰīw kʰǎw tā.nāːw sǐː] ; Malay : Banjaran Tanah Seri/Banjaran Tenang Sari ) is the geographical name of a roughly 1,700 km long mountain chain, part of the Indo-Malayan mountain system in Southeast Asia . Despite their relatively scant altitude these mountains form an effective barrier between Thailand and Myanmar in their northern and central region. There are only two main transnational roads and cross-border points between Kanchanaburi and Tak , at

222-680: A Bell UH-1 Iroquois , that had occurred two days earlier while looking for illegal loggers in Kaeng Krachan National Park near the Burmese border west of Phetchaburi . The Black Hawk helicopter crashed near 978 m high Yage Taung mountain in the Tanintharyi National Park zone in Burma, close to the border with Thailand. A third helicopter, a Bell 212 , also crashed in the same area on Sunday, 25 July

333-510: A pitch-register language like Shanghainese . There are four contrastive tones in Burmese. In the following table, the tones are shown marked on the vowel /a/ as an example. For example, the following words are distinguished from each other only on the basis of tone: In syllables ending with /ɰ̃/ , the checked tone is excluded: In spoken Burmese, some linguists classify two real tones (there are four nominal tones transcribed in written Burmese), "high" (applied to words that terminate with

444-645: A subject–object–verb word order. It is a member of the Lolo-Burmese grouping of the Sino-Tibetan language family . The Burmese alphabet is ultimately descended from a Brahmic script , either the Kadamba or Pallava alphabets. Burmese belongs to the Southern Burmish branch of the Sino-Tibetan languages , of which Burmese is the most widely spoken of the non- Sinitic languages. Burmese

555-614: A concentrated belt that stretches east–west except in East China where it is tilted east-northeast over Korea and Japan. The seasonal rain is known as Meiyu in China, Jangma in Korea, and Bai-u in Japan, with the latter two resembling frontal rain. The onset of the summer monsoon is marked by a period of premonsoonal rain over South China and Taiwan in early May. From May through August,

666-548: A few miles further east close to the Kaeng Krachan Reservoir . Superstitious people blamed the three consecutive crashes on the fact that, according to Thai folklore , the densely forested mountains of the Tenasserim Range have strong guardian spirits . Burmese language Burmese is a tonal , pitch-register , and syllable-timed language , largely monosyllabic and agglutinative with

777-622: A few sub-systems, such as the Indian Subcontinental Monsoon which affects the Indian subcontinent and surrounding regions including Nepal, and the East Asian Monsoon which affects southern China, Taiwan , Korea and parts of Japan. The southwestern summer monsoons occur from June through September. The Thar Desert and adjoining areas of the northern and central Indian subcontinent heat up considerably during

888-554: A large-scale sea breeze caused by higher temperature over land than in the ocean. This is no longer considered as the cause and the monsoon is now considered a planetary-scale phenomenon involving the annual migration of the Intertropical Convergence Zone between its northern and southern limits. The limits of the ITCZ vary according to the land–sea heating contrast and it is thought that the northern extent of

999-550: A lesser extent, Burmese has also imported words from Sanskrit (religion), Hindi (food, administration, and shipping), and Chinese (games and food). Burmese has also imported a handful of words from other European languages such as Portuguese . Here is a sample of loan words found in Burmese: Since the end of British rule, the Burmese government has attempted to limit usage of Western loans (especially from English) by coining new words ( neologisms ). For instance, for

1110-547: A low pressure system known as a monsoon trough develops over South-East Asia and Australasia and winds are directed toward Australia. In the Philippines, northeast monsoon is called Amihan . The East Asian monsoon affects large parts of Indochina , the Philippines , China, Taiwan , Korea, Japan, and Siberia . It is characterised by a warm, rainy summer monsoon and a cold, dry winter monsoon. The rain occurs in

1221-413: A lower temperature than the land, and the air above it retains a higher pressure. This difference in pressure causes sea breezes to blow from the ocean to the land, bringing moist air inland. This moist air rises to a higher altitude over land and then it flows back toward the ocean (thus completing the cycle). However, when the air rises, and while it is still over the land, the air cools . This decreases

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1332-674: A monk]", Lower Burmese speakers use [sʰʊ́ɰ̃] instead of [sʰwáɰ̃] , which is the pronunciation used in Upper Burma. The standard dialect is represented by the Yangon dialect because of the modern city's media influence and economic clout. In the past, the Mandalay dialect represented standard Burmese. The most noticeable feature of the Mandalay dialect is its use of the first person pronoun ကျွန်တော် , kya.nau [tɕənɔ̀] by both men and women, whereas in Yangon,

1443-661: A period of global cooling and sea level fall. The EASM was weaker during cold intervals of glacial periods such as the Last Glacial Maximum (LGM) and stronger during interglacials and warm intervals of glacial periods. Another EAWM intensification event occurred 2.6 million years ago, followed by yet another one around 1.0 million years ago. During Dansgaard–Oeschger events , the EASM grew in strength, but it has been suggested to have decreased in strength during Heinrich events . The EASM expanded its influence deeper into

1554-819: A railway line between Bangkok and that harbor. The southern section of this extensive chain of mountains runs along the Kra Isthmus into the Malay Peninsula almost reaching Singapore . Many rivers have their source in these mountains, but none of them are very long. This mountain chain is named after the Tenasserim Region (Tanintharyi) in Burma and its name in Thai is Thio Khao Tanaosi , also spelt as Tanawsri , Tanao Sri , Tanaw Sri or in Malay as Tanah Seri . All those names are corrupted form of

1665-535: A seasonal reversing wind accompanied by corresponding changes in precipitation but is now used to describe seasonal changes in 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 rainy phase of a seasonally changing pattern, although technically there

1776-466: A stop or check, high-rising pitch) and "ordinary" (unchecked and non-glottal words, with falling or lower pitch), with those tones encompassing a variety of pitches. The "ordinary" tone consists of a range of pitches. Linguist L. F. Taylor concluded that "conversational rhythm and euphonic intonation possess importance" not found in related tonal languages and that "its tonal system is now in an advanced state of decay." The syllable structure of Burmese

1887-411: A strong tendency to diverge, subside and cause drought. Similar rainfall is caused when moist ocean air is lifted upwards by mountains, surface heating, convergence at the surface, divergence aloft, or from storm-produced outflows at the surface. However the lifting occurs, the air cools due to expansion in lower pressure, and this produces condensation . The monsoon of western Sub-Saharan Africa

1998-628: Is mutual intelligibility among Burmese dialects, as they share a common set of tones, consonant clusters, and written script. However, several Burmese dialects differ substantially from standard Burmese with respect to vocabulary, lexical particles, and rhymes. Spoken Burmese is remarkably uniform among Burmese speakers, particularly those living in the Irrawaddy valley, all of whom use variants of Standard Burmese. The standard dialect of Burmese (the Mandalay - Yangon dialect continuum ) comes from

2109-400: Is C(G)V((V)C), which is to say the onset consists of a consonant optionally followed by a glide , and the rime consists of a monophthong alone, a monophthong with a consonant, or a diphthong with a consonant. The only consonants that can stand in the coda are /ʔ/ and /ɰ̃/ . Some representative words are: Monsoon A monsoon ( / m ɒ n ˈ s uː n / ) is traditionally

2220-470: Is a big problem at Kaeng Krachan National Park , with the authorities being unable to control the poachers. Some park officials are allegedly involved in the trade of elephant parts. This range forms a natural border between Burma and Thailand, but it was crossed in 1759 by Burmese troops led by Alaungpaya and his son Hsinbyushin during the Burmese–Siamese War (1759–1760) . The Burmese battle plan

2331-706: 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 West African , Asian– Australian , the North American , and South American monsoons. The term was first used in English in British India and neighboring countries to refer to the big seasonal winds blowing from the Bay of Bengal and Arabian Sea in

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2442-666: Is directly of "cyclonic" (i.e., monsoon-driven) origin (as opposed to " local convection "). The effects also extend westwards to the Mediterranean, where however the impact of the monsoon is to induce drought via the Rodwell-Hoskins mechanism . Around September, with the sun retreating south, the northern landmass of the Indian subcontinent begins to cool off rapidly, and air pressure begins to build over northern India. The Indian Ocean and its surrounding atmosphere still hold their heat, causing cold wind to sweep down from

2553-610: Is known to many as the Summer , Southwest , Mexican or Arizona monsoon. It is also sometimes called the Desert monsoon as a large part of the affected area are the Mojave and Sonoran deserts . However, it is controversial whether the North and South American weather patterns with incomplete wind reversal should be counted as true monsoons. The Asian monsoons may be classified into

2664-756: Is located in the Khao Sam Roi Yot limestone mountains, a coastal offshoot of the main Tenasserim range and Nam Tok Huay Yang National Park is another park in Prachuap Khiri Khan Province that is located on the Thai side by the border area between 100 and 1200 metres above sea level. In Malaysia the main protected areas in the range area are Endau-Rompin National Park , Gunung Ledang National Park , Taman Negara and Selangor State Park . The killing of wild elephants

2775-442: Is pronounced [mõ̀ũndã́ĩ] . The vowels of Burmese are: The monophthongs /e/ , /o/ , /ə/ , /ɛ/ and /ɔ/ occur only in open syllables (those without a syllable coda ); the diphthongs /ei/ , /ou/ , /ai/ and /au/ occur only in closed syllables (those with a syllable coda). /ə/ only occurs in a minor syllable , and is the only vowel that is permitted in a minor syllable (see below). The close vowels /i/ and /u/ and

2886-523: Is the result of the seasonal shifts of the Intertropical Convergence Zone and the great seasonal temperature and humidity differences between the Sahara and the equatorial Atlantic Ocean. The ITCZ migrates northward from the equatorial Atlantic in February, reaches western Africa on or near June 22, then moves back to the south by October. The dry, northeasterly trade winds , and their more extreme form,

2997-584: Is the value of the four native final nasals: ⟨မ်⟩ /m/ , ⟨န်⟩ /n/ , ⟨ဉ်⟩ /ɲ/ , ⟨င်⟩ /ŋ/ , as well as the retroflex ⟨ဏ⟩ /ɳ/ (used in Pali loans) and nasalisation mark anusvara demonstrated here above ka (က → ကံ) which most often stands in for a homorganic nasal word medially as in တံခါး tankhá 'door', and တံတား tantá 'bridge', or else replaces final -m ⟨မ်⟩ in both Pali and native vocabulary, especially after

3108-638: Is the word "moon", which can be လ la̰ (native Tibeto-Burman), စန္ဒာ/စန်း [sàndà]/[sã́] (derivatives of Pali canda 'moon'), or သော်တာ [t̪ɔ̀ dà] (Sanskrit). The consonants of Burmese are as follows: According to Jenny & San San Hnin Tun (2016 :15), contrary to their use of symbols θ and ð, consonants of သ are dental stops ( /t̪, d̪/ ), rather than fricatives ( /θ, ð/ ) or affricates. These phonemes, alongside /sʰ/ , are prone to merger with /t, d, s/ . An alveolar /ɹ/ can occur as an alternate of /j/ in some loanwords. The final nasal /ɰ̃/

3219-491: The [ ɹ ] sound, which has become [ j ] in standard Burmese. Moreover, Arakanese features a variety of vowel differences, including the merger of the ဧ [e] and ဣ [i] vowels. Hence, a word like "blood" သွေး is pronounced [θw é ] in standard Burmese and [θw í ] in Arakanese. The Burmese language's early forms include Old Burmese and Middle Burmese . Old Burmese dates from

3330-588: The /l/ medial, which is otherwise only found in Old Burmese inscriptions. They also often reduce the intensity of the glottal stop . Beik has 250,000 speakers while Tavoyan has 400,000. The grammatical constructs of Burmese dialects in Southern Myanmar show greater Mon influence than Standard Burmese. The most pronounced feature of the Arakanese language of Rakhine State is its retention of

3441-523: The Andaman Sea . Further south the Kraburi River forms the southern border between Thailand and Burma. Great extensions of these hills are covered with dense tropical moist forests . Usually the western slopes are more densely forested than the eastern for they receive more abundant monsoon rains. The range is home to several distinct ecoregions. The Dawna and other northern ranges are in

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3552-637: The Arabian Sea and that of the wind-blown dust in the Loess Plateau of China, many geologists believe the monsoon first became strong around 8 million years ago. More recently, studies of plant fossils in China and new long-duration sediment records from the South China Sea led to a timing of the monsoon beginning 15–20 million years ago and linked to early Tibetan uplift. Testing of this hypothesis awaits deep ocean sampling by

3663-529: The Burma Railway between Bangkok and Yangon , Hellfire Pass in the Tenasserim Range was a particularly difficult section of the line to build. It was the largest rock cutting on the railway, also known as the "Death Railway", coupled with its general remoteness and the lack of proper construction tools during building. The Australian , British , Dutch , other allied prisoners of war, along with Chinese , Malay and Tamil labourers, were required by

3774-475: The Burmese alphabet began employing cursive-style circular letters typically used in palm-leaf manuscripts , as opposed to the traditional square block-form letters used in earlier periods. The orthographic conventions used in written Burmese today can largely be traced back to Middle Burmese. Modern Burmese emerged in the mid-18th century. By this time, male literacy in Burma stood at nearly 50%, which enabled

3885-618: The English language in the colonial educational system, especially in higher education. In the 1930s, the Burmese language saw a linguistic revival, precipitated by the establishment of an independent University of Rangoon in 1920 and the inception of a Burmese language major at the university by Pe Maung Tin , modeled on Anglo Saxon language studies at the University of Oxford. Student protests in December of that year, triggered by

3996-756: The Hadley circulation during boreal winter. It is associated with the development of the Siberian High and the movement of the heating maxima from the Northern Hemisphere to the Southern Hemisphere. North-easterly winds flow down Southeast Asia, are turned north-westerly/westerly by Borneo topography towards Australia. This forms a cyclonic circulation vortex over Borneo, which together with descending cold surges of winter air from higher latitudes, cause significant weather phenomena in

4107-636: The Himalayas and Indo-Gangetic Plain towards the vast spans of the Indian Ocean south of the Deccan peninsula. This is known as the Northeast Monsoon or Retreating Monsoon. While travelling towards the Indian Ocean, the cold dry wind picks up some moisture from the Bay of Bengal and pours it over peninsular India and parts of Sri Lanka . Cities like Chennai , which get less rain from

4218-557: The Indonesian Throughflow generally warms the Indian Ocean. Thus these five intervals could probably be those of considerable lowering of SST in the Indian Ocean and would have influenced Indian monsoon intensity. During the weak LC, there is the possibility of reduced intensity of the Indian winter monsoon and strong summer monsoon, because of change in the Indian Ocean dipole due to reduction in net heat input to

4329-627: The Integrated Ocean Drilling Program . The monsoon has varied significantly in strength since this time, largely linked to global climate change , especially the cycle of the Pleistocene ice ages. A study of Asian monsoonal climate cycles from 123,200 to 121,210 years BP, during the Eemian interglacial, suggests that they had an average duration of around 64 years, with the minimum duration being around 50 years and

4440-546: The Kawkareik Pass in the Tenasserim Range. A road was cut across the mountains by Japanese military engineers, but many infantry units crossed the range on foot in an arduous march through the forests and cliffs. This road was impracticable during the rainy season, when mud and rivulets made advance difficult for the Japanese Infantry and leeches abounded. Between 1942 and 1943, during the construction of

4551-746: The Kayah-Karen montane rain forests ecoregion. The Tenasserim-South Thailand semi-evergreen rain forests cover the Bilauktaung range and the Isthmus of Kra, and extend to the coast on both sides of the isthmus. The Kayah-Karen montane rain forests and Tenasserim-South Thailand semi-evergreen forests together form the Kayah-Karen/Tenasserim moist forests ecoregion which is included in the Global 200 list of ecoregions identified by

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4662-723: The Mon people , who until recently formed the majority in Lower Burma . Most Mon loanwords are so well assimilated that they are not distinguished as loanwords, as Burmese and Mon were used interchangeably for several centuries in pre-colonial Burma. Mon loans are often related to flora, fauna, administration, textiles, foods, boats, crafts, architecture, and music. As a natural consequence of British rule in Burma , English has been another major source of vocabulary, especially with regard to technology, measurements, and modern institutions. English loanwords tend to take one of three forms: To

4773-534: The Myanma Salonpaung Thatpon Kyan ( မြန်မာ စာလုံးပေါင်း သတ်ပုံ ကျမ်း ), was compiled in 1978 by the commission. Burmese is a diglossic language with two distinguishable registers (or diglossic varieties ): The literary form of Burmese retains archaic and conservative grammatical structures and modifiers (including affixes and pronouns) no longer used in the colloquial form. Literary Burmese, which has not changed significantly since

4884-945: The Phetchaburi River flow eastwards from the range towards the Gulf of Siam . The westernmost range is separated from the Tenasserim coast by the Three Pagodas Fault . West of it lie the Dawna Range, the Karen Hills and the valleys of the Salween and the Gyaing . Southwards on the western side, the Ye , Heinze , Dawei (Tavoy), Great Tenasserim (Tanintharyi) and the Lenya rivers are relatively short and flow into

4995-506: The Pyu language . These indirect borrowings can be traced back to orthographic idiosyncrasies in these loanwords, such as the Burmese word "to worship", which is spelt ပူဇော် ( pūjo ) instead of ပူဇာ ( pūjā ), as would be expected by the original Pali orthography. The transition to Middle Burmese occurred in the 16th century. The transition to Middle Burmese included phonological changes (e.g. mergers of sound pairs that were distinct in Old Burmese) as well as accompanying changes in

5106-432: The Sierra Madre Occidental as well as Arizona , New Mexico , Nevada , Utah , Colorado , West Texas and California . It pushes as far west as the Peninsular Ranges and Transverse Ranges of Southern California, but rarely reaches the coastal strip (a wall of desert thunderstorms only a half-hour's drive away is a common summer sight from the sunny skies along the coast during the monsoon). The North American monsoon

5217-429: The Tenasserim white-bellied rat and the Tenasserim lutung , as well as a number of bird species and the Tenasserim Mountain bent-toed gecko . Among the fishes in the streams and rivulets of the range the emperor loach and the Tenasserim garra deserve mention. The Tanintharyi National Park and the Tanintharyi Nature Reserve were established in 2005, and the Lenya National Park was proposed in 2002 and 2004, on

5328-405: The Three Pagodas Pass and at Mae Sot . The latter is located beyond the northern end of the range, where the Tenasserim Hills meet the Dawna Range . Minor cross-border points are Sing Khon , near Prachuap Khiri Khan , as well as Bong Ti and Phu Nam Ron west of Kanchanaburi . The latter is expected to gain in importance if the planned Dawei Port Project goes ahead, along with a highway and

5439-399: The World Wildlife Fund (WWF) as priorities for conservation. The Kangar-Pattani floristic boundary runs across the peninsula in southern Thailand and northernmost Malaysia, marking the boundary between the large biogeographic regions of Indochina to the north and Sundaland and Malesia to the south. The forests north of the boundary are characterized by seasonally-deciduous trees, while

5550-421: The harmattan , are interrupted by the northern shift in the ITCZ and resultant southerly, rain-bearing winds during the summer. The semiarid Sahel and Sudan depend upon this pattern for most of their precipitation. The North American monsoon ( NAM ) occurs from late June or early July into September, originating over Mexico and spreading into the southwest United States by mid-July. It affects Mexico along

5661-455: The return of the westerlies ) is the result of a resurgence of westerly winds from the Atlantic, where they become loaded with wind and rain. These westerly winds are a common phenomenon during the European winter, but they ease as spring approaches in late March and through April and May. The winds pick up again in June, which is why this phenomenon is also referred to as "the return of the westerlies". The rain usually arrives in two waves, at

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5772-413: The 11th to the 16th century ( Pagan to Ava dynasties); Middle Burmese from the 16th to the 18th century ( Toungoo to early Konbaung dynasties); modern Burmese from the mid-18th century to the present. Word order , grammatical structure, and vocabulary have remained markedly stable well into Modern Burmese, with the exception of lexical content (e.g., function words ). The earliest attested form of

5883-457: The 13th century, is the register of Burmese taught in schools. In most cases, the corresponding affixes in the literary and spoken forms are totally unrelated to each other. Examples of this phenomenon include the following lexical terms: Historically the literary register was preferred for written Burmese on the grounds that "the spoken style lacks gravity, authority, dignity". In the mid-1960s, some Burmese writers spearheaded efforts to abandon

5994-410: The 19th century, in addition to concomitant economic and political instability in Upper Burma (e.g., increased tax burdens from the Burmese crown, British rice production incentives, etc.) also accelerated the migration of Burmese speakers from Upper Burma into Lower Burma. British rule in Burma eroded the strategic and economic importance of the Burmese language; Burmese was effectively subordinated to

6105-471: The British in the lead-up to the independence of Burma in 1948. The 1948 Constitution of Burma prescribed Burmese as the official language of the newly independent nation. The Burma Translation Society and Rangoon University's Department of Translation and Publication were established in 1947 and 1948, respectively, with the joint goal of modernizing the Burmese language in order to replace English across all disciplines. Anti-colonial sentiment throughout

6216-501: The Buddhist clergy (monks) from the laity ( householders ), especially when speaking to or about bhikkhus (monks). The following are examples of varying vocabulary used for Buddhist clergy and for laity: Burmese primarily has a monosyllabic received Sino-Tibetan vocabulary. Nonetheless, many words, especially loanwords from Indo-European languages like English, are polysyllabic, and others, from Mon, an Austroasiatic language, are sesquisyllabic . Burmese loanwords are overwhelmingly in

6327-450: The Burmese language into Lower Burma also coincided with the emergence of Modern Burmese. As late as the mid-1700s, Mon , an Austroasiatic language, was the principal language of Lower Burma, employed by the Mon people who inhabited the region. Lower Burma's shift from Mon to Burmese was accelerated by the Burmese-speaking Konbaung Dynasty 's victory over the Mon-speaking Restored Hanthawaddy Kingdom in 1757. By 1830, an estimated 90% of

6438-407: The Burmese language is called Old Burmese , dating to the 11th and 12th century stone inscriptions of Pagan . The earliest evidence of the Burmese alphabet is dated to 1035, while a casting made in the 18th century of an old stone inscription points to 984. Owing to the linguistic prestige of Old Pyu in the Pagan Kingdom era, Old Burmese borrowed a substantial corpus of vocabulary from Pali via

6549-447: The Burmese side in order to implement habitat conservation , but illegal logging driven by greed and corruption is an ongoing problem on both sides of the border. On the Thai side the Kaeng Krachan National Park was demarcated already in 1981, covering parts of the districts of Nong Ya Plong , Kaeng Krachan and Tha Yang of Phetchaburi Province , and of Hua Hin of Prachuap Khiri Khan Province . The Khao Sam Roi Yot National Park

6660-488: The EAWM occurred 5.5 million years ago. The EAWM was still significantly weaker relative to today between 4.3 and 3.8 million years ago but abruptly became more intense around 3.8 million years ago as crustal stretching widened the Tsushima Strait and enabled greater inflow of the warm Tsushima Current into the Sea of Japan. Circa 3.0 million years ago, the EAWM became more stable, having previously been more variable and inconsistent, in addition to being enhanced further amidst

6771-516: The East Asian monsoon's strength began to wane, weakening from that point until the present day. A particularly notable weakening took place ~3,000 BP. The location of the EASM shifted multiple times over the course of the Holocene: first, it moved southward between 12,000 and 8,000 BP, followed by an expansion to the north between approximately 8,000 and 4,000 BP, and most recently retreated southward once more between 4,000 and 0 BP. The January ITCZ migrated further south to its present location during

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6882-405: The GDP and employs 70% of the population) is heavily dependent on the rains, for growing crops especially like cotton , rice , oilseeds and coarse grains. A delay of a few days in the arrival of the monsoon can badly affect the economy, as evidenced in the numerous droughts in India in the 1990s. The monsoon is widely welcomed and appreciated by city-dwellers as well, for it provides relief from

6993-427: The Indian Ocean increased the intensity of monsoons. In 2018, a study of the SAM's variability over the past million years found that precipitation resulting from the monsoon was significantly reduced during glacial periods compared to interglacial periods like the present day. The Indian Summer Monsoon (ISM) underwent several intensifications during the warming following the Last Glacial Maximum, specifically during

7104-574: The Indian Ocean through the Indonesian Throughflow. Thus a better understanding of the possible links between El Niño , Western Pacific Warm Pool, Indonesian Throughflow, wind pattern off western Australia, and ice volume expansion and contraction can be obtained by studying the behaviour of the LC during Quaternary at close stratigraphic intervals. The South American summer monsoon (SASM) is known to have become weakened during Dansgaard–Oeschger events. The SASM has been suggested to have been enhanced during Heinrich events. Monsoons were once considered as

7215-432: The Irrawaddy River valley. Regional differences between speakers from Upper Burma (e.g., Mandalay dialect), called anya tha ( အညာသား ) and speakers from Lower Burma (e.g., Yangon dialect), called auk tha ( အောက်သား ), largely occur in vocabulary choice, not in pronunciation. Minor lexical and pronunciation differences exist throughout the Irrawaddy River valley. For instance, for the term ဆွမ်း , "food offering [to

7326-477: The Japanese to complete the cutting of the stretch. 69 men were beaten to death by Japanese and Korean guards in the six weeks it took to build the railway pass, and many more died from cholera , dysentery , starvation , and exhaustion (Wigmore 568). On 19 July 2011, a Royal Thai Army Sikorsky UH-60 Black Hawk helicopter crashed in these mountains, killing 9. The chopper had been sent out to recover five bodies of victims of another helicopter crash involving

7437-408: The Kra Isthmus. Eastwards, in Kanchanaburi Province on the Thai side, the mountain range is crossed by the Khwae Yai River and the Khwae Noi River . In this area small hill ridges alternate with narrow valleys that are often only about 2 km wide and further east there are only isolated hills, where the range ends in the Central Plain of Thailand. Further south the Phachi , the Pranburi and

7548-413: The Middle Miocene, strengthening the summer monsoon of Australia that had previously been weaker. Five episodes during the Quaternary at 2.22 Ma ( PL-1), 1.83 Ma (PL-2), 0.68 Ma (PL-3), 0.45 Ma (PL-4) and 0.04 Ma (PL-5) were identified which showed a weakening of the Leeuwin Current (LC). The weakening of the LC would have an effect on the sea surface temperature (SST) field in the Indian Ocean, as

7659-431: The OB vowel *u e.g. ငံ ngam 'salty', သုံး thóum ('three; use'), and ဆုံး sóum 'end'. It does not, however, apply to ⟨ည်⟩ which is never realised as a nasal, but rather as an open front vowel [iː] [eː] or [ɛː] . The final nasal is usually realised as nasalisation of the vowel. It may also allophonically appear as a homorganic nasal before stops. For example, in /mòʊɰ̃dáɪɰ̃/ ('storm'), which

7770-422: The Southwest Monsoon first hits the Western Ghats of the coastal state of Kerala , India, thus making this area the first state in India to receive rain from the Southwest Monsoon. This branch of the monsoon moves northwards along the Western Ghats ( Konkan and Goa ) with precipitation on coastal areas, west of the Western Ghats. The eastern areas of the Western Ghats do not receive much rain from this monsoon as

7881-535: The Southwest Monsoon, receive rain from this Monsoon. About 50% to 60% of the rain received by the state of Tamil Nadu is from the Northeast Monsoon. In Southern Asia, the northeastern monsoons take place from October to December when the surface high-pressure system is strongest. The jet stream in this region splits into the southern subtropical jet and the polar jet. The subtropical flow directs northeasterly winds to blow across southern Asia, creating dry air streams which produce clear skies over India. Meanwhile,

7992-725: The Sundaland forests have more year-round rainfall and the trees are mostly evergreen. The ranges in Peninsular Malaysia are part of the Peninsular Malaysian montane rain forests ecoregion. The Tenasserim Hills form the habitat for a number of endangered species, including the Gurney's pitta , endemic to Thailand and Burma, as well as the Asian elephant and tiger . The Sumatran rhinoceros has been reported in

8103-491: The adoption of neologisms. An example is the word "university", formerly ယူနီဗာစတီ [jùnìbàsətì] , from English university , now တက္ကသိုလ် [tɛʔkət̪ò] , a Pali-derived neologism recently created by the Burmese government and derived from the Pali spelling of Taxila ( တက္ကသီလ Takkasīla ), an ancient university town in modern-day Pakistan. Some words in Burmese may have many synonyms, each having certain usages, such as formal, literary, colloquial, and poetic. One example

8214-438: The air's ability to hold water , and this causes precipitation over the land. This is why summer monsoons cause so much rain over land. In the colder months, the cycle is reversed. Then the land cools faster than the oceans and the air over the land has higher pressure than air over the ocean. This causes the air over the land to flow to the ocean. When humid air rises over the ocean, it cools, and this causes precipitation over

8325-635: The arrival at the Eastern Himalayas, the winds turns towards the west, travelling over the Indo-Gangetic Plain at a rate of roughly 1–2 weeks per state, pouring rain all along its way. June 1 is regarded as the date of onset of the monsoon in India, as indicated by the arrival of the monsoon in the southernmost state of Kerala. The monsoon accounts for nearly 80% of the rainfall in India. Indian agriculture (which accounts for 25% of

8436-507: The beginning of June, and again in mid- to late June. The European monsoon is not a monsoon in the traditional sense in that it doesn't meet all the requirements to be classified as such. Instead, the return of the westerlies is more regarded as a conveyor belt that delivers a series of low-pressure centres to Western Europe where they create unsettled weather. These storms generally feature significantly lower-than-average temperatures, fierce rain or hail, thunder, and strong winds. The return of

8547-713: The climax of summer heat in June. However, the roads take a battering every year. Often houses and streets are waterlogged and slums are flooded despite drainage systems. A lack of city infrastructure coupled with changing climate patterns causes severe economic loss including damage to property and loss of lives, as evidenced in the 2005 flooding in Mumbai that brought the city to a standstill. Bangladesh and certain regions of India like Assam and West Bengal , also frequently experience heavy floods during this season. Recently, areas in India that used to receive scanty rainfall throughout

8658-525: The close portions of the diphthongs are somewhat mid-centralized ( [ɪ, ʊ] ) in closed syllables, i.e. before /ɰ̃/ and /ʔ/ . Thus နှစ် /n̥iʔ/ ('two') is phonetically [n̥ɪʔ] and ကြောင် /tɕàũ/ ('cat') is phonetically [tɕàʊ̃] . Burmese is a tonal language , which means phonemic contrasts can be made on the basis of the tone of a vowel. In Burmese, these contrasts involve not only pitch , but also phonation , intensity (loudness), duration, and vowel quality. However, some linguists consider Burmese

8769-604: The country. These varieties include the Yaw , Palaw, Myeik (Merguese), Tavoyan and Intha dialects . Despite substantial vocabulary and pronunciation differences, there is mutual intelligibility among most Burmese dialects. Below is a summary of lexical similarity between major Burmese dialects: Dialects in Tanintharyi Region , including Palaw, Merguese, and Tavoyan, are especially conservative in comparison to Standard Burmese. The Tavoyan and Intha dialects have preserved

8880-669: The early post-independence era led to a reactionary switch from English to Burmese as the national medium of education, a process that was accelerated by the Burmese Way to Socialism . In August 1963, the socialist Union Revolutionary Government established the Literary and Translation Commission (the immediate precursor of the Myanmar Language Commission ) to standardize Burmese spelling, diction, composition, and terminology. The latest spelling authority, named

8991-401: The earth by conduction and not by convection. Therefore, bodies of water stay at a more even temperature, while land temperatures are more variable. During warmer months sunlight heats the surfaces of both land and oceans, but land temperatures rise more quickly. As the land's surface becomes warmer, the air above it expands and an area of low pressure develops. Meanwhile, the ocean remains at

9102-598: The form of nouns . Historically, Pali , the liturgical language of Theravada Buddhism , had a profound influence on Burmese vocabulary. Burmese has readily adopted words of Pali origin; this may be due to phonotactic similarities between the two languages, alongside the fact that the script used for Burmese can be used to reproduce Pali spellings with complete accuracy. Pali loanwords are often related to religion, government, arts, and science. Burmese loanwords from Pali primarily take four forms: Burmese has also adapted numerous words from Mon, traditionally spoken by

9213-459: The hot summers. This causes a low pressure area over the northern and central Indian subcontinent. To fill this void, the moisture-laden winds from the Indian Ocean rush into the subcontinent. These winds, rich in moisture, are drawn towards the Himalayas . The Himalayas act like a high wall, blocking the winds from passing into Central Asia, and forcing them to rise. As the clouds rise, their temperature drops, and precipitation occurs . Some areas of

9324-652: The interior of Asia as sea levels rose following the LGM; it also underwent a period of intensification during the Middle Holocene, around 6,000 years ago, due to orbital forcing made more intense by the fact that the Sahara at the time was much more vegetated and emitted less dust. This Middle Holocene interval of maximum EASM was associated with an expansion of temperate deciduous forest steppe and temperate mixed forest steppe in northern China. By around 5,000 to 4,500 BP,

9435-522: The introduction of English into matriculation examinations , fueled growing demand for Burmese to become the medium of education in British Burma; a short-lived but symbolic parallel system of "national schools" that taught in Burmese, was subsequently launched. The role and prominence of the Burmese language in public life and institutions was championed by Burmese nationalists, intertwined with their demands for greater autonomy and independence from

9546-515: The literary form, asserting that the spoken vernacular form ought to be used. Some Burmese linguists such as Minn Latt , a Czech academic, proposed moving away from the high form of Burmese altogether. Although the literary form is heavily used in written and official contexts (literary and scholarly works, radio news broadcasts, and novels), the recent trend has been to accommodate the spoken form in informal written contexts. Nowadays, television news broadcasts, comics, and commercial publications use

9657-618: The maximum approximately 80 years, similar to today. A study of marine plankton suggested that the South Asian Monsoon (SAM) strengthened around 5 million years ago. Then, during ice periods, the sea level fell and the Indonesian Seaway closed. When this happened, cold waters in the Pacific were impeded from flowing into the Indian Ocean. It is believed that the resulting increase in sea surface temperatures in

9768-610: The monsoon in South Asia is influenced by the high Tibetan Plateau. These temperature imbalances happen because oceans and land absorb heat in different ways. Over oceans, the air temperature remains relatively stable for two reasons: water has a relatively high heat capacity (3.9 to 4.2 J g K ), and because both conduction and convection will equilibrate a hot or cold surface with deeper water (up to 50 metres). In contrast, dirt, sand, and rocks have lower heat capacities (0.19 to 0.35 J g K ), and they can only transmit heat into

9879-513: The monsoon is not a simple response to heating but a more complex interaction of topography, wind and sea, as demonstrated by its abrupt rather than gradual withdrawal from the region. The Australian monsoon (the "Wet") occurs in the southern summer when the monsoon trough develops over Northern Australia . Over three-quarters of annual rainfall in Northern Australia falls during this time. The European Monsoon (more commonly known as

9990-495: The northern section of the wider range. There are records from the north of Tenasserim proper , where there were numerous reports in 1962, to Kota Tinggi in the south where a rhino was captured in 1994. The Endau-Rompin National Park in Malaysia has the largest remaining Sumatran rhinoceros population in the range. Other species include the sambar deer , barking deer , serow , red goral , leopard , Kitti's hog-nosed bat ,

10101-408: The oceans. (The cool air then flows towards the land to complete the cycle.) Most summer monsoons have a dominant westerly component and a strong tendency to ascend and produce copious amounts of rain (because of the condensation of water vapor in the rising air). The intensity and duration, however, are not uniform from year to year. Winter monsoons, by contrast, have a dominant easterly component and

10212-498: The original Malay Tanah Seri , which means "glowing land" or from tanah sirih meaning " betel land". The Tenasserim Hills are part of a long granite mountain ridge that is older than the Himalayas . Further south from the 16th parallel, the Shan Hills break up into narrow steep-sided ranges, the Dawna Range in the west and, parallel to it at the southern end, the peninsular Tenasserim Mountains that extend southwards along

10323-649: The population in Lower Burma self-identified as Burmese-speaking Bamars; huge swaths of former Mon-speaking territory, from the Irrawaddy Delta to upriver in the north, spanning Bassein (now Pathein) and Rangoon (now Yangon) to Tharrawaddy, Toungoo, Prome (now Pyay), and Henzada (now Hinthada), were now Burmese-speaking. The language shift has been ascribed to a combination of population displacement, intermarriage, and voluntary changes in self-identification among increasingly Mon–Burmese bilingual populations in

10434-425: The region. Standardized tone marking in written Burmese was not achieved until the 18th century. From the 19th century onward, orthographers created spellers to reform Burmese spelling, because of ambiguities that arose over transcribing sounds that had been merged. British rule saw continued efforts to standardize Burmese spelling through dictionaries and spellers. Britain's gradual annexation of Burma throughout

10545-446: The region. Examples are the formation of a rare low-latitude tropical storm in 2001, Tropical Storm Vamei , and the devastating flood of Jakarta in 2007. The onset of the monsoon over Australia tends to follow the heating maxima down Vietnam and the Malay Peninsula (September), to Sumatra , Borneo and the Philippines (October), to Java , Sulawesi (November), Irian Jaya and northern Australia (December, January). However,

10656-510: The said pronoun is used only by male speakers while ကျွန်မ , kya.ma. [tɕəma̰] is used by female speakers. Moreover, with regard to kinship terminology , Upper Burmese speakers differentiate the maternal and paternal sides of a family, whereas Lower Burmese speakers do not. The Mon language has also influenced subtle grammatical differences between the varieties of Burmese spoken in Lower and Upper Burma. In Lower Burmese varieties,

10767-666: The southwest bringing heavy rainfall to the area. The etymology of the word monsoon is not wholly certain. The English monsoon came from Portuguese monção ultimately from Arabic موسم ( mawsim , "season"), "perhaps partly via early modern Dutch monson ". Strengthening of the Asian monsoon has been linked to the uplift of the Tibetan Plateau after the collision of the Indian subcontinent and Asia around 50 million years ago. Because of studies of records from

10878-764: The spoken form or a combination of the spoken and simpler, less ornate formal forms. The following sample sentence reveals that differences between literary and spoken Burmese mostly occur in affixes: Burmese has politeness levels and honorifics that take the speaker's status and age in relation to the audience into account. The suffix ပါ pa is frequently used after a verb to express politeness. Moreover, Burmese pronouns relay varying degrees of deference or respect. In many instances, polite speech (e.g., addressing teachers, officials, or elders) employs feudal-era third person pronouns or kinship terms in lieu of first- and second-person pronouns. Furthermore, with regard to vocabulary choice, spoken Burmese clearly distinguishes

10989-562: The subcontinent receive up to 10,000 mm (390 in) of rain annually. The southwest monsoon is generally expected to begin around the beginning of June and fade away by the end of September. The moisture-laden winds on reaching the southernmost point of the Indian Peninsula , due to its topography, become divided into two parts: the Arabian Sea Branch and the Bay of Bengal Branch . The Arabian Sea Branch of

11100-546: The summer monsoon shifts through a series of dry and rainy phases as the rain belt moves northward, beginning over Indochina and the South China Sea (May), to the Yangtze River Basin and Japan (June) and finally to northern China and Korea (July). When the monsoon ends in August, the rain belt moves back to southern China. The rainy season occurs from September to February and it is a major source of energy for

11211-633: The time intervals corresponding to 16,100–14,600 BP, 13,600–13,000 BP, and 12,400–10,400 BP as indicated by vegetation changes in the Tibetan Plateau displaying increases in humidity brought by an intensifying ISM. Though the ISM was relatively weak for much of the Late Holocene, significant glacial accumulation in the Himalayas still occurred due to cold temperatures brought by westerlies from

11322-448: The traditional homeland of Burmese speakers. The 1891 Census of India , conducted five years after the annexation of the entire Konbaung Kingdom , found that the former kingdom had an "unusually high male literacy" rate of 62.5% for Upper Burmans aged 25 and above. For all of British Burma , the literacy rate was 49% for men and 5.5% for women (by contrast, British India more broadly had a male literacy rate of 8.44%). The expansion of

11433-425: The underlying orthography . From the 1500s onward, Burmese kingdoms saw substantial gains in the populace's literacy rate , which manifested itself in greater participation of laymen in scribing and composing legal and historical documents, domains that were traditionally the domain of Buddhist monks, and drove the ensuing proliferation of Burmese literature , both in terms of genres and works. During this period,

11544-527: The verb ပေး ('to give') is colloquially used as a permissive causative marker, like in other Southeast Asian languages, but unlike in other Tibeto-Burman languages. This usage is hardly used in Upper Burmese varieties, and is considered a sub-standard construct. More distinctive non-standard varieties emerge as one moves farther away from the Irrawaddy River valley toward peripheral areas of

11655-794: The west. During the Middle Miocene , the July ITCZ, the zone of rainfall maximum, migrated northwards, increasing precipitation over southern China during the East Asian Summer Monsoon (EASM) while making Indochina drier. During the Late Miocene Global Cooling (LMCG), from 7.9 to 5.8 million years ago, the East Asian Winter Monsoon (EAWM) became stronger as the subarctic front shifted southwards. An abrupt intensification of

11766-466: The wide circulation of legal texts, royal chronicles , and religious texts. A major reason for the uniformity of the Burmese language was the near-universal presence of Buddhist monasteries (called kyaung ) in Burmese villages. These kyaung served as the foundation of the pre-colonial monastic education system, which fostered uniformity of the language throughout the Upper Irrawaddy valley,

11877-719: The wind does not cross the Western Ghats. The Bay of Bengal Branch of Southwest Monsoon flows over the Bay of Bengal heading towards north-east India and Bengal , picking up more moisture from the Bay of Bengal. The winds arrive at the Eastern Himalayas with large amounts of rain. Mawsynram , situated on the southern slopes of the Khasi Hills in Meghalaya , India, is one of the wettest places on Earth. After

11988-410: The word "television", Burmese publications are mandated to use the term ရုပ်မြင်သံကြား (lit. 'see picture, hear sound') in lieu of တယ်လီဗီးရှင်း , a direct English transliteration. Another example is the word "vehicle", which is officially ယာဉ် [jɪ̃̀] (derived from Pali) but ကား [ká] (from English car ) in spoken Burmese. Some previously common English loanwords have fallen out of use with

12099-604: The year, like the Thar Desert , have surprisingly ended up receiving floods due to the prolonged monsoon season. The influence of the Southwest Monsoon is felt as far north as in China's Xinjiang . It is estimated that about 70% of all precipitation in the central part of the Tian Shan Mountains falls during the three summer months, when the region is under the monsoon influence; about 70% of that

12210-839: Was the fifth of the Sino-Tibetan languages to develop a writing system, after Classical Chinese , Pyu , Old Tibetan and Tangut . The majority of Burmese speakers, who live throughout the Irrawaddy River Valley, use a number of largely similar dialects, while a minority speak non-standard dialects found in the peripheral areas of the country. These dialects include: Arakanese in Rakhine State and Marma in Bangladesh are also sometimes considered dialects of Burmese and sometimes as separate languages. Despite vocabulary and pronunciation differences, there

12321-695: Was to go around the heavily defended Siamese positions along shorter, more direct invasion routes. The invasion force overran relatively thin Siamese defenses in the coast, crossed the Tenasserim Hills to the shore of the Gulf of Siam , and turned north towards Ayutthaya . In January 1942, at the beginning of the Japanese conquest of Burma , the main body of the Japanese 33d Division began the main attack towards Rangoon westward from Thailand across

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