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102-611: The town lies on the Mekong River opposite Chiang Khong in Thailand. The Fourth Thai-Lao Friendship Bridge at Ban Houayxay, which opened in December 2013 and replaced ferry service across the river, is now the northernmost road border crossing between the two countries. Asian Highway 3 , which runs through Ban Houayxay, extends north to Yunnan Province of China and south to Chiang Rai Province of Thailand . Houayxay has

204-512: A domestic airport (HOE) with regular flights to Vientiane and Luang Prabang (depending on the season). The town is the starting point for many boats (speed and slow boats, freighters, luxury cruisers for tourists and others) on the Mekong River to Pakbeng , Luang Prabang and other destinations. Houayxay is also home to the Gibbon Experience, another highlight for tourists. It is a series of ziplines and treehouses providing

306-555: A drainage area of 795,000 km (307,000 sq mi), discharging 475 km (114 cu mi) of water annually. From its headwaters in the Tibetan Plateau , the river runs through Southwest China (where it is officially called the Lancang River ), Myanmar , Laos , Thailand , Cambodia , and southern Vietnam . The extreme seasonal variations in flow and the presence of rapids and waterfalls in

408-404: A tone number at the end of individual syllables. For example, tóng is written tong . Each tone can be denoted with its numeral the order listed above. The neutral tone can either be denoted with no numeral, with 0, or with 5. Briefly, tone marks should always be placed in the order a, e, i, o, u, ü , with the only exceptions being iu and io where the tone mark is placed on

510-619: A Chinese government project in the 1950s. Zhou, often called "the father of pinyin", worked as a banker in New York when he decided to return to China to help rebuild the country after the People's Republic was established. Earlier attempts to romanize Chinese writing were mostly abandoned in 1944. Zhou became an economics professor in Shanghai, and when the Ministry of Education created

612-689: A GB recommendation in 1996, and were last updated in 2012. In practice, however, published materials in China now often space pinyin syllable by syllable. According to Victor H. Mair , this practice became widespread after the Script Reform Committee, previously under direct control of the State Council , had its power greatly weakened in 1985 when it was renamed the State Language Commission and placed under

714-789: A connection to the South China Sea. Although the hydraulic relationships between the Mekong and the Tonle Sap Great Lake systems during the Holocene are not well understood, it is clear that between 9,000 and 7,500 years ago the confluence of the Tonle Sap and the Mekong was in proximity to the South China Sea. The present river morphology of the Mekong Delta developed over the last 6,000 years. During this period,

816-604: A generic word for major rivers. To the early European traders, the Mekong River was also known as Mekon River , May-Kiang River and Cambodia River . The local names for the river include: The Mekong rises as the Za Qu ( Tibetan : རྫ་ཆུ་ , Wylie : rDza chu , ZYPY : Za qu ; Chinese : 扎曲 ; pinyin : Zā Qū ) and soon becomes known as the Lancang River ( simplified Chinese : 澜沧江 ; traditional Chinese : 瀾滄 江 ; pinyin : Láncāng Jiāng , from

918-478: A high evaporation rate means it is classified as a semi-arid region. Consequently, although the Mun and Chi basins drain 15% of the entire Mekong basin, they only contribute 6% of the average annual flow. Sandy and saline soils are the most common soil types, which makes much of the land unsuitable for wet rice cultivation. In spite of poor fertility, however, agriculture is intensive. Glutinous rice, maize, and cassava are

1020-416: A major distinction in the low-flow hydrology of the river. One fraction comes from melting snow in China and Tibet and the rest from over-season catchment storage in the lower basin. This has implications for the occurrence of drought conditions. For example, if runoff from melting snow in any given year is very low, then flows upstream of Vientiane - Nong Khai would be lower. In a large river system like

1122-591: A maximum of about 4.5 m (15 ft) above present levels in the early Holocene about 8 ka. At this time the shoreline of the South China Sea almost reached Phnom Penh and cores recovered from near Angkor Borei contained sediments deposited under the influence of tides, and salt marsh and mangrove swamp deposits. Sediments deposited in the Tonle Sap Great Lake about this time (7.9–7.3 ka) also show indications of marine influence, suggesting

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1224-589: A stretch of some 2,200 km (1,400 mi). Here, it drops 4,500 m (14,800 ft) before it enters the lower basin where the borders of Thailand, Laos, China, and Myanmar come together in the Golden Triangle. Downstream from the Golden Triangle, the river flows for a further 2,600 km (1,600 mi) through Laos, Thailand, and Cambodia before entering the South China Sea via a complex delta system in Vietnam . The upper basin makes up 24% of

1326-400: A trailing -r is considered part of a syllable (a phenomenon known as erhua ). The latter case, though a common practice in some sub-dialects, is rarely used in official publications. Even though most initials contain a consonant, finals are not always simple vowels, especially in compound finals ( 复韵母 ; 複韻母 ; fùyùnmǔ ), i.e. when a "medial" is placed in front of the final. For example,

1428-511: A unique overnight experience. Fort Carnot , an ancient French fort in ruins, sits on a hill overlooking the town and the Mekong River. Mekong River The Mekong or Mekong River is a trans-boundary river in East Asia and Southeast Asia . It is the world's twelfth-longest river and the third-longest in Asia with an estimated length of 4,909 km (3,050 mi) and

1530-497: Is attached as a grammatical suffix . A Chinese syllable ending with any other consonant either is from a non-Mandarin language (a southern Chinese language such as Cantonese , reflecting final consonants in Old Chinese ), or indicates the use of a non-pinyin romanization system, such as one that uses final consonants to indicate tones. Technically, i, u, ü without a following vowel are finals, not medials, and therefore take

1632-662: Is based on the phonological system of Beijing Mandarin. Other romanization schemes have been devised to transcribe those other Chinese varieties, such as Jyutping for Cantonese and Pe̍h-ōe-jī for Hokkien . Based on the "Chinese Romanization" section of ISO 7098:2015, pinyin tone marks should use the symbols from Combining Diacritical Marks , as opposed by the use of Spacing Modifier Letters in bopomofo. Lowercase letters with tone marks are included in GB 2312 and their uppercase counterparts are included in JIS X 0212 ; thus Unicode includes all

1734-493: Is both a medial and a coda, the nucleus may be dropped from writing. In this case, when the coda is a consonant n or ng , the only vowel left is the medial i, u , or ü , and so this takes the diacritic. However, when the coda is a vowel, it is the coda rather than the medial which takes the diacritic in the absence of a written nucleus. This occurs with syllables ending in -ui (from wei : wèi → -uì ) and in -iu (from you : yòu → -iù ). That is, in

1836-411: Is difficult because it is not present as a simple key on many keyboard layouts. For these reasons v is sometimes used instead by convention. For example, it is common for cellphones to use v instead of ü . Additionally, some stores in China use v instead of ü in the transliteration of their names. The drawback is a lack of precomposed characters and limited font support for combining accents on

1938-477: Is flooded during the rainy season. The impact of road embankments and similar infrastructure developments on the movement of this flood water is an increasingly important consequence of development. Table 2 summarises the mean annual flows along the mainstream. The mean annual flow entering the lower Mekong from China is equivalent to a relatively modest 450 mm (18 in) depth of runoff. Downstream of Vientiane this increases to over 600 mm (24 in) as

2040-550: Is generally described in terms of sound pairs of two initials ( 声母 ; 聲母 ; shēngmǔ ) and finals ( 韵母 ; 韻母 ; yùnmǔ ). This is distinct from the concept of consonant and vowel sounds as basic units in traditional (and most other phonetic systems used to describe the Chinese language). Every syllable in Standard Chinese can be described as a pair of one initial and one final, except for the special syllable er or when

2142-528: Is heterogeneous and active, and is the major factor controlling the course of rivers and the landscapes they carve out. The elevation of the Tibetan Plateau during the Tertiary period was an important factor in the genesis of the south-west monsoon , which is the dominant climatic control influencing the hydrology of the Mekong Basin. Understanding the nature and timing of the elevation of Tibet (and

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2244-531: Is little evidence from the last 45 years of data of any systematic changes in the hydrological regime of the Mekong. The internal drainage patterns of the Mekong are unusual among those of large rivers. Most large river systems that drain the interiors of continents, such as the Amazon , Congo , and Mississippi , have relatively simple dendritic tributary networks that resemble a branching tree. Typically, such patterns develop in basins with gentle slopes where

2346-571: Is not limited only to pinyin, since many languages that use the Latin alphabet natively also assign different values to the same letters. A recent study on Chinese writing and literacy concluded, "By and large, pinyin represents the Chinese sounds better than the Wade–Giles system, and does so with fewer extra marks." As pinyin is a phonetic writing system for modern Standard Chinese , it is not designed to replace characters for writing Literary Chinese ,

2448-614: Is not ordinarily reflected in pinyin spelling. Standard Chinese has many polysyllabic words. Like in other writing systems using the Latin alphabet, spacing in pinyin is officially based on word boundaries. However, there are often ambiguities in partitioning a word. The Basic Rules of the Chinese Phonetic Alphabet Orthography were put into effect in 1988 by the National Educational and National Language commissions. These rules became

2550-409: Is rarely used due to difficulty of entering it on computers. (Starts with the vowel sound in f a ther and ends in the velar nasal ; like s ong in some dialects of American English) An umlaut is added to ⟨ u ⟩ when it occurs after the initials ⟨ l ⟩ and ⟨ n ⟩ when necessary in order to represent the sound [y] . This is necessary in order to distinguish

2652-504: Is spelled in terms of an optional initial and a final , each of which is represented by one or more letters. Initials are initial consonants, whereas finals are all possible combinations of medials ( semivowels coming before the vowel), a nucleus vowel, and coda (final vowel or consonant). Diacritics are used to indicate the four tones found in Standard Chinese, though these are often omitted in various contexts, such as when spelling Chinese names in non-Chinese texts. Hanyu Pinyin

2754-675: Is the beginning of the Mekong Delta. The two rivers, the Bassac to the west and the Mekong to the east, enter Vietnam shortly after this. In Vietnam, the Bassac is called the Hậu River (Sông Hậu or Hậu Giang); the main, eastern, branch of the Mekong is called the Tiền River or Tiền Giang. In Vietnam, distributaries of the eastern (main, Mekong) branch include the Mỹ Tho River , the Ba Lai River ,

2856-691: Is the official romanisation system used in China, Singapore, Taiwan, and by the United Nations . Its use has become common when transliterating Standard Chinese mostly regardless of region, though it is less ubiquitous in Taiwan. It is used to teach Standard Chinese, normally written with Chinese characters , to students already familiar with the Latin alphabet . Pinyin is also used by various input methods on computers and to categorize entries in some Chinese dictionaries . In pinyin, each Chinese syllable

2958-630: Is transcribed in pinyin simply as yú , not as * yǘ . This practice is opposed to Wade–Giles, which always uses ü , and Tongyong Pinyin , which always uses yu . Whereas Wade–Giles needs the umlaut to distinguish between chü (pinyin ju ) and chu (pinyin zhu ), this ambiguity does not arise with pinyin, so the more convenient form ju is used instead of jü . Genuine ambiguities only happen with nu / nü and lu / lü , which are then distinguished by an umlaut. Many fonts or output methods do not support an umlaut for ü or cannot place tone marks on top of ü . Likewise, using ü in input methods

3060-475: Is used for large rivers and Khong is the proper name referred to as "River Khong". However, Khong is an archaic word meaning "river", loaned from Austroasiatic languages , such as Vietnamese sông (from * krong ) and Mon kruŋ "river", which led to Chinese 江 whose Old Chinese pronunciation has been reconstructed as /*kˤroŋ/ and which long served as the proper name of the Yangtze before becoming

3162-570: The Central Highlands of Vietnam) therefore helps explain the provenance of sediment reaching the delta and the Tonle Sap Great Lake today. Studies of the provenance of sediments in the Mekong delta reveal a major switch in the source of sediments about eight million years ago (Ma) . From 36 to 8 Ma the bulk (76%) of the sediments deposited in the delta came from erosion of the bedrock in the Three Rivers Area . From 8 Ma to

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3264-591: The Hàm Luông River , and the Cổ Chiên River . The Mekong Basin is frequently divided into two parts: the "upper Mekong basin" comprising those parts of the basin in Tibet , Yunnan and eastern Myanmar , and the "lower Mekong basin" from Yunnan downstream from China to the South China Sea . From the point where it rises to its mouth, the most precipitous drop in the Mekong occurs in the upper Mekong basin,

3366-495: The International Phonetic Alphabet (IPA) transcription, the second indicates pinyin for a standalone (no-initial) form, and the third indicates pinyin for a combination with an initial. Other than finals modified by an -r , which are omitted, the following is an exhaustive table of all possible finals. The only syllable-final consonants in Standard Chinese are -n , -ng , and -r , the last of which

3468-422: The Ministry of Education . Mair claims that proponents of Chinese characters in the educational bureaucracy "became alarmed that word-based pinyin was becoming a de facto alternative to Chinese characters as a script for writing Mandarin and demanded that all pinyin syllables be written separately." Pinyin superseded older romanization systems such as Wade–Giles and postal romanization , and replaced bopomofo as

3570-429: The Ministry of Public Security standardized the practice to use "LYU" and "NYU" in passports. Although nüe written as nue , and lüe written as lue are not ambiguous, nue or lue are not correct according to the rules; nüe and lüe should be used instead. However, some Chinese input methods support both nve / lve (typing v for ü ) and nue / lue . The pinyin system also uses four diacritics to mark

3672-591: The Nam Ngum , Nam Theun , Nam Hinboun, Se Bang Fai , Se Bang Hieng and Se Done Rivers. The Mun - Chi river system from the right bank in Thailand enters the mainstream within this reach. Reach 4: Pakse to Kratie . The main hydrological contributions to the mainstream in this reach come from the Se Kong , Se San , and Sre Pok catchments. Together, these rivers make up the largest hydrological sub-component of

3774-465: The Richter magnitude scale and is unlikely to cause material damage. The difficulty of navigating the river has meant that it has divided, rather than united, the people who live near it. The earliest known settlements date to 210 BCE, with Ban Chiang being an excellent example of early Iron Age culture. The earliest recorded civilization was the 1st century Indianised -Khmer culture of Funan , in

3876-826: The Three Parallel Rivers Area in the Hengduan Mountains , along with the Yangtze to its east and the Salween River (Nu Jiang in Chinese) to its west. Then the Mekong meets the China–Myanmar border and flows about 10 km (6 mi) along that border until it reaches the tripoint of China, Myanmar and Laos . From there it flows southwest and forms the border of Myanmar and Laos for about 100 km (60 mi) until it arrives at

3978-587: The Tonlé Sap . When the Mekong is low, the Tonle Sap is a tributary : water flows from the lake and river into the Mekong. When the Mekong floods, the flow reverses: the floodwaters of the Mekong flow up the Tonle Sap. Immediately after the Sap River joins the Mekong by Phnom Penh, the Bassac River branches off the right (west) bank. The Bassac River is the first and main distributary of the Mekong. This

4080-633: The Yunnan component makes up almost 30% of the average dry season flow. A major concern is that the ongoing and planned expansion of dams and reservoirs on the Mekong mainstream in Yunnan could have a significant effect on the low-flow regime of the lower Mekong basin system. Reach 2: Chiang Saen to Vientiane and Nong Khai . This reach is almost entirely mountainous and covered with natural forest although there has been widespread slash and burn agriculture. Although this reach cannot be termed "unspoiled",

4182-488: The tones of Mandarin . In the pinyin system, four main tones of Mandarin are shown by diacritics: ā, á, ǎ, and à. There is no symbol or diacritic for the neutral tone: a. The diacritic is placed over the letter that represents the syllable nucleus , unless that letter is missing. Tones are used in Hanyu Pinyin symbols, and they do not appear in Chinese characters. Tones are written on the finals of Chinese pinyin. If

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4284-547: The 1950s to around 50% in the mid-1990s. Agricultural expansion and population pressure are the major reasons for land use and landscape change. Both drought and flood are common hazards in the Delta, which many people believe is the most sensitive to upstream hydrological change. Table 1: Country share of Mekong River Basin (MRB) and water flows By taking into account hydrological regimes, physiography land use, and existing, planned and potential resource developments,

4386-685: The Committee for the Reform of the Chinese Written Language in 1955, Premier Zhou Enlai assigned him the task of developing a new romanization system, despite the fact that he was not a linguist by trade. Hanyu Pinyin incorporated different aspects from existing systems, including Gwoyeu Romatzyh (1928), Latinxua Sin Wenz (1931), and the diacritics from bopomofo (1918). "I'm not the father of pinyin", Zhou said years later; "I'm

4488-529: The Eyes and Ears of Western Literati' ( 西儒耳目資 ; Xīrú ěrmù zī )) in Hangzhou. Neither book had any influence among the contemporary Chinese literati, and the romanizations they introduced primarily were useful for Westerners. During the late Qing, the reformer Song Shu (1862–1910) proposed that China adopt a phonetic writing system. A student of the scholars Yu Yue and Zhang Taiyan , Song had observed

4590-780: The Great Lake via the Tonle Sap River . Phnom Penh also marks the beginning of the delta system of the Mekong River. Here the mainstream begins to break up into an increasing number of branches. In Cambodia, wet rice is the main crop and is grown on the flood plains of the Tonle Sap, Mekong, and Bassac (the Mekong delta distributary known as the Hậu in Vietnam) Rivers. More than half of Cambodia remains covered with mixed evergreen and deciduous broadleaf forest, but forest cover has decreased from 73% in 1973 to 63% in 1993. Here,

4692-692: The Hanyu Pinyin romanization system instead of earlier romanization systems; this change followed the Joint Communiqué on the Establishment of Diplomatic Relations between the United States and China in 1979. In 2001, the Chinese government issued the National Common Language Law , providing a legal basis for applying pinyin. The current specification of the orthography is GB/T 16159–2012. Chinese phonology

4794-734: The Kingdom of Thailand which is the mechanism for cooperation with regard to riverine trade on the upper stretches of the Mekong. The Mekong basin is one of the richest areas of biodiversity in the world. Only the Amazon boasts a higher level of bio-diversity. Biota estimates for the Greater Mekong Subregion (GMS) include 20,000 plant species, 430 mammals, 1,200 birds, 800 reptiles and amphibians, and an estimated 850 freshwater fish species (excluding euryhaline species mainly found in salt or brackish water, as well as introduced species ). The most species rich orders among

4896-478: The Laos-Thailand border for some 850 km (530 mi) as it flows first east, passing the capital of Laos, Vientiane , then turns south. A second time, the river leaves the border and flows east into Laos soon passing the city of Pakse . Thereafter, it turns and runs more or less directly south, crossing into Cambodia . At Phnom Penh the river is joined on the right bank by the river and lake system

4998-630: The Mekong delta. Excavations at Oc Eo , near modern An Giang , have found coins from as far away as the Roman Empire . This was succeeded by the Khmer culture Chenla state around the 5th century. The Khmer empire of Angkor was the last great Indianized state in the region. From around the time of the fall of the Khmer empire, the Mekong was the front line between the emergent states of Siam and Tonkin (North Vietnam), with Laos and Cambodia, then on

5100-467: The Mekong is divided into six distinct reaches : Reach 1: Lancang Jiang or Upper Mekong River in China . In this part of the river, the major source of water flowing into the river comes from melting snow on the Tibetan plateau . This volume of water is sometimes called the "Yunnan component" and plays an important role in the low-flow hydrology of the lower mainstream. Even as far downstream as Kratie,

5202-465: The Mekong make navigation difficult. Even so, the river is a major trade route between Tibet and Southeast Asia. The construction of hydroelectric dams along the Mekong in the 2000s through the 2020s has caused serious problems for the river's ecosystem , including the exacerbation of drought . The Mekong was originally called Mae Nam Khong from a contracted form of Tai shortened to Mae Khong . In Thai and Lao, Mae Nam ("Mother of Water[s]")

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5304-655: The Mekong, seasonal flows can be quite variable from year to year. Although the pattern of the annual hydrograph is fairly predictable, its magnitude is not. The average monthly flows along the mainstream are listed in Table 3, providing an indication of their range and variability from year to year. At Pakse , for example, flood season flows during August would exceed 20,000 m /s (5,300,000 US gal/s) nine years out of ten, but exceed 34,000 m /s (9,000,000 US gal/s) only one year in ten. Table 3: Mekong Mainstream monthly discharge, 1960–2004 (m /s). There

5406-442: The Mun and Chi Rivers, that drain a large part of northeast Thailand. Laos lies almost entirely within the lower Mekong basin. Its climate, landscape and land use are the major factors shaping the hydrology of the river. The mountainous landscape means that only 16% of the country is farmed under lowland terrace or upland shifting cultivation . With upland shifting agriculture (slash and burn), soils recover within 10 to 20 years but

5508-601: The Private Use Areas, and some input methods (e.g. Sogou Pinyin) also outputs the Private Use Areas code point instead of the original character. As the superset GB 18030 changed the mappings of ⟨ḿ⟩ and ⟨ǹ⟩ , this has caused an issue where the input methods and font files use different encoding standards, and thus the input and output of both characters are mixed up. Other symbols are used in pinyin are as follows: The spelling of Chinese geographical or personal names in pinyin has become

5610-559: The United Nations began using it in 1986. Taiwan adopted Hanyu Pinyin as its official romanization system in 2009, replacing Tongyong Pinyin . Matteo Ricci , a Jesuit missionary in China, wrote the first book that used the Latin alphabet to write Chinese, entitled Xizi Qiji ( 西字奇蹟 ; 'Miracle of Western Letters') and published in Beijing in 1605. Twenty years later, fellow Jesuit Nicolas Trigault published 'Aid to

5712-416: The absence of a written nucleus the finals have priority for receiving the tone marker, as long as they are vowels; if not, the medial takes the diacritic. An algorithm to find the correct vowel letter (when there is more than one) is as follows: Worded differently, The above can be summarized as the following table. The vowel letter taking the tone mark is indicated by the fourth-tone mark. Tone sandhi

5814-474: The basin are small. Only 14 have catchment areas that exceed 1,000 km (400 sq mi), yet the greatest amount of loss of forest cover in the entire river system per square kilometer has occurred in this region due to heavy unchecked demand for natural resources. In the south of Yunnan, in Simao and Xishuangbanna Prefectures, the river changes as the valley opens out, the floodplain becomes wider, and

5916-543: The basis of Pinyin standard later after incorporating a wide range of feedback and further revisions. The first edition of Hanyu Pinyin was approved and officially adopted at the Fifth Session of the 1st National People's Congress on 11 February 1958. It was then introduced to primary schools as a way to teach Standard Chinese pronunciation and used to improve the literacy rate among adults. Despite its formal promulgation, pinyin did not become widely used until after

6018-428: The border of Laos with Thailand. Khon Pi Long is a series of rapids along a 1.6 km (1.0 mi) section of the Mekong River dividing Chiang Rai and Bokeo Province in Laos. The name of the rapids means 'where the ghost lost its way'. It then turns east into the interior of Laos, flowing first east and then south for some 400 km (250 mi) before meeting the border with Thailand again. Once more, it defines

6120-417: The coast, torn between their influence. The first European to encounter the Mekong was the Portuguese António de Faria in 1540. A European map of 1563 depicts the river, although even by then little was known of the river upstream of the delta. European interest was sporadic: the Spanish and Portuguese mounted some missionary and trade expeditions, while the Dutch Gerrit van Wuysthoff led an expedition up

6222-499: The common accented characters from pinyin. Other punctuation mark and symbols in Chinese are to use the equivalent symbol in English noted in to GB 15834. According to GB 16159, all accented letters are required to have both uppercase and lowercase characters as per their normal counterparts. GBK has mapped two characters ⟨ḿ⟩ and ⟨ǹ⟩ to Private Use Areas in Unicode respectively, thus some fonts (e.g. SimSun) that adhere to GBK include both characters in

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6324-440: The delta advanced 200 km (120 mi) over the continental shelf of the South China Sea, covering an area of more than 62,500 km (24,100 sq mi). From 5.3 to 3.5 ka the delta advanced across a broad embayment formed between higher ground near the Cambodian border and uplands north of Ho Chi Minh City . During this phase of its development the delta was sheltered from the wave action of long-shore currents and

6426-452: The delta. For much of its length the Mekong flows through bedrock channels, i.e., channels that are confined or constrained by bedrock or old alluvium in the bed and riverbanks. Geomorphologic features normally associated with the alluvial stretches of mature rivers, such as meanders , oxbow lakes , cut-offs, and extensive floodplains are restricted to a short stretch of the mainstream around Vientiane and downstream of Kratie where

6528-410: The effect of the kana syllabaries and Western learning during his visits to Japan. While Song did not himself propose a transliteration system for Chinese, his discussion ultimately led to a proliferation of proposed schemes. The Wade–Giles system was produced by Thomas Wade in 1859, and further improved by Herbert Giles , presented in Chinese–English Dictionary (1892). It was popular, and

6630-416: The finals rather than as part of them; this convention is followed in the chart of finals below. The conventional lexicographical order derived from bopomofo is: In each cell below, the pinyin letters assigned to each initial are accompanied by their phonetic realizations in brackets, notated according to the International Phonetic Alphabet . In each cell below, the first line indicates

6732-439: The freshwater fish in the river basin are cypriniforms (377 species) and catfish (92 species). Pinyin Hanyu Pinyin , or simply pinyin , is the most common romanization system for Standard Chinese . In official documents, it is referred to as the Chinese Phonetic Alphabet . Hanyu ( 汉语 ; 漢語 ) literally means ' Han language'—that is, the Chinese language—while pinyin literally means 'spelled sounds'. Pinyin

6834-434: The front high rounded vowel in lü (e.g. 驴 ; 驢 ; 'donkey') from the back high rounded vowel in lu (e.g. 炉 ; 爐 ; 'oven'). Tonal markers are placed above the umlaut, as in lǘ . However, the ü is not used in the other contexts where it could represent a front high rounded vowel, namely after the letters j , q , x , and y . For example, the sound of the word for 'fish' ( 鱼 ; 魚 )

6936-529: The hydrological impacts of land cover changes induced by the Vietnam War were quantified in two sub-catchments of the lower Mekong River basin. Loss of forest cover in the Thai areas of the lower basin has been the highest of all the lower Mekong countries over the past 60 years. On the Khorat Plateau , which includes the Mun and Chi tributary systems, forest cover was reduced from 42% in 1961 to 13% in 1993. Although this part of northeast Thailand has an annual rainfall of more than 1,000 mm (40 in),

7038-437: The hydrological response is perhaps the most natural and undisturbed of all the lower basin. Many hydrological aspects of the lower basin start to change rapidly at the downstream boundary of this reach. On 19 July 2019 this reach of the river dropped to its lowest level in a century. Officials are particularly concerned as July is in the wet season, when mainstream flows are abundant historically. Locals are blaming low water on

7140-548: The letter v , ( v̄ v́ v̌ v̀ ). This also presents a problem in transcribing names for use on passports, affecting people with names that consist of the sound lü or nü , particularly people with the surname 吕 ( Lǚ ), a fairly common surname, particularly compared to the surnames 陆 ( Lù ), 鲁 ( Lǔ ), 卢 ( Lú ) and 路 ( Lù ). Previously, the practice varied among different passport issuing offices, with some transcribing as "LV" and "NV" while others used "LU" and "NU". On 10 July 2012,

7242-437: The lower basin from Yunnan make up about 15% of the wet season flow at Kratie . This rises to 40% during the dry season, even this far downstream. During the wet season, the proportion of average flow coming from Yunnan rapidly decreases downstream of Chiang Saen, from 70% to less than 20% at Kratie. The dry season contribution from Yunnan is much more significant. The major portion of the balance comes from Laos, which points to

7344-524: The lower basin. Over 25% of the mean annual flow volume to the mainstream at Kratie comes from these three river basins. They are the key element in the hydrology of this part of the system, especially to the Tonle Sap flow reversal. Reach 5: Kratie to Phnom Penh . This reach includes the hydraulic complexities of the Cambodian floodplain, the Tonle Sap and the Great Lake. By this stage, over 95% of

7446-415: The medials [ i ] and [ u ] are pronounced with such tight openings at the beginning of a final that some native Chinese speakers (especially when singing) pronounce yī ( 衣 ; 'clothes'), officially pronounced /í/ , as /jí/ and wéi ( 围 ; 圍 ; 'to enclose'), officially pronounced /uěi/ , as /wěi/ or /wuěi/ . Often these medials are treated as separate from

7548-772: The method of Chinese phonetic instruction in mainland China . The ISO adopted pinyin as the standard romanization for modern Chinese in 1982 (ISO 7098:1982, superseded by ISO 7098:2015). The United Nations followed suit in 1986. It has also been accepted by the government of Singapore , the United States's Library of Congress , the American Library Association , and many other international institutions. Pinyin assigns some Latin letters sound values which are quite different from those of most languages. This has drawn some criticism as it may lead to confusion when uninformed speakers apply either native or English assumed pronunciations to words. However, this problem

7650-495: The most common way to transcribe them in English. Pinyin has also become the dominant Chinese input method in mainland China, in contrast to Taiwan, where bopomofo is most commonly used. Families outside of Taiwan who speak Mandarin as a mother tongue use pinyin to help children associate characters with spoken words which they already know. Chinese families outside of Taiwan who speak some other language as their mother tongue use

7752-611: The newly constructed Xayaburi Dam , as it enters its test phase prior to the start of commercial operation in October 2019. Reach 3: Vientiane and Nong Khai to Pakse . The boundary between Reach 2 and 3 is where the Mekong hydrology starts to change. Reach 2 is dominated in both wet and dry seasons by the Yunnan Component. Reach 3 is increasingly influenced by contributions from the large left bank tributaries in Laos, namely

7854-749: The old name of Lao kingdom Lan Xang ; the characters may also be literally understood as "turbulent green river"). It originates in the " three rivers source area " on the Tibetan Plateau in the Sanjiangyuan National Nature Reserve . The reserve protects the headwaters of, from north to south, the Yellow (Huang He), the Yangtze , and the Mekong Rivers. It flows through the Tibetan Autonomous Region and then southeast into Yunnan Province, and then

7956-727: The present, however, the contribution from the Three Rivers Area fell to 40%, while that from the Central Highlands rose from 11 to 51%. One of the most striking conclusions of provenance studies is the small contribution of sediment from the other parts of the Mekong basin, notably the Khorat Plateau, the uplands of northern Laos and northern Thailand, and the mountain ranges south of the Three Rivers area. The last glacial period came to an abrupt end about 19,000 years ago (19 ka ) when sea levels rose rapidly, reaching

8058-436: The principal crops. Drought is by far the major hydrological hazard in this region. As the Mekong enters Cambodia, over 95% of its flows have already joined the river. From here on downstream the terrain is flat and water levels rather than flow volumes determine the movement of water across the landscape. The seasonal cycle of changing water levels at Phnom Penh results in the unique "flow reversal" of water into and out of

8160-796: The principal left bank tributaries enter the mainstream, mainly the Nam Ngum and Nam Theun. The flow level falls again, even with the right bank entry of the Mun-Chi system from Thailand. Although the Mun–Chi basin drains 20% of the lower system, average annual runoff is only 250 mm (10 in). Runoff in the mainstream increases again with the entry from the left bank of the Se Kong from southern Laos and Se San and Sre Pok from Vietnam and Cambodia. Table 2: Lower Mekong Mainstream annual flow (1960 to 2004) at selected sites. Flows at Chiang Saen entering

8262-495: The river as far as Vientiane in 1641–42. The French invaded the region in the mid-19th century, capturing Saigon in 1861, and establishing a protectorate over Cambodia in 1863. The first systematic European exploration began with the French Mekong Expedition led by Ernest Doudard de Lagrée and Francis Garnier , which ascended the river from its mouth to Yunnan between 1866 and 1868. Their chief finding

8364-400: The river becomes wider and slower. Major tributary systems develop in the lower basin. These systems can be separated into two groups: tributaries that contribute to the major wet season flows, and tributaries that drain low relief regions of lower rainfall. The first group are left bank tributaries that drain the high rainfall areas of Laos. The second group are those on the right bank, mainly

8466-448: The river develops alluvial channels that are free of control exerted by the underlying bedrock. The Mekong basin is not normally considered a seismically active area as much of the basin is underlain by the relatively stable continental block. Nonetheless, the parts of the basin in northern Laos , northern Thailand , Myanmar and China do experience frequent earthquakes and tremors. The magnitude of these earthquakes rarely exceeds 6.5 on

8568-464: The river landscape is flat. Small changes in water level determine the direction of water movement, including the large-scale reversal of flow into and out of the Tonle Sap basin from the Mekong River. The Mekong Delta in Vietnam is farmed intensively and has little natural vegetation left. Forest cover is less than 10%. In the Central Highlands of Vietnam, forest cover was reduced from over 95% in

8670-418: The second vowel instead. Pinyin tone marks appear primarily above the syllable nucleus—e.g. as in kuài , where k is the initial, u the medial, a the nucleus, and i is the coda. There is an exception for syllabic nasals like /m/ , where the nucleus of the syllable is a consonant: there, the diacritic will be carried by a written dummy vowel. When the nucleus is / ə / (written e or o ), and there

8772-608: The son of pinyin. It's [the result of] a long tradition from the later years of the Qing dynasty down to today. But we restudied the problem and revisited it and made it more perfect." An initial draft was authored in January 1956 by Ye Laishi , Lu Zhiwei and Zhou Youguang. A revised Pinyin scheme was proposed by Wang Li, Lu Zhiwei and Li Jinxi, and became the main focus of discussion among the group of Chinese linguists in June 1956, forming

8874-498: The standard written language prior to the early 1900s. In particular, Chinese characters retain semantic cues that help distinguish differently pronounced words in the ancient classical language that are now homophones in Mandarin. Thus, Chinese characters remain indispensable for recording and transmitting the corpus of Chinese writing from the past. Pinyin is not designed to transcribe varieties other than Standard Chinese, which

8976-633: The support of the Office of Weapons Removal and Abatement within the US State Department Bureau of Political-Military Affairs , to conduct underwater explosive removal. The many maps of the river basin produced throughout recorded history reflect the region's changing human geography and politics. In 1995, Laos, Thailand, Cambodia, and Vietnam established the Mekong River Commission (MRC) to manage and coordinate

9078-527: The tone mark is written over an i , then it replaces the tittle, as in yī . In dictionaries, neutral tone may be indicated by a dot preceding the syllable—e.g. ·ma . When a neutral tone syllable has an alternative pronunciation in another tone, a combination of tone marks may be used: zhī·dào ( 知道 ) may be pronounced either zhīdào or zhīdao . Before the advent of computers, many typewriter fonts did not contain vowels with macron or caron diacritics. Tones were thus represented by placing

9180-565: The tone marks, but they are more concisely displayed as above. In addition, ê [ɛ] ( 欸 ; 誒 ) and syllabic nasals m ( 呒 , 呣 ), n ( 嗯 , 唔 ), ng ( 嗯 , 𠮾 ) are used as interjections or in neologisms ; for example, pinyin defines the names of several pinyin letters using -ê finals. According to the Scheme for the Chinese Phonetic Alphabet , ng can be abbreviated with the shorthand ŋ . However, this shorthand

9282-409: The total area and contributes 15–20% of the water that flows into the Mekong River. The catchment here is steep and narrow with Soil erosion being a major problem and as a result of this, approximately 50% of the sediment in the river comes from the upper basin. In Yunnan Province in China, the river and its tributaries are confined by narrow, deep gorges. The tributary river systems in this part of

9384-572: The total flow has entered the Mekong system. The focus turns from hydrology and water discharge to the assessment of water level, over- bank storage and flooding and the hydrodynamics that determine the timing, duration and volume of the seasonal flow reversal into and out of the Great Lake. Reach 6: Phnom Penh to the South China Sea . Here the mainstream divides into a complex and increasingly controlled and artificial system of branches and canals. Key features of flow behaviour are tidal influences and salt water intrusion. Every year, 35–50% of this reach

9486-616: The tripoint of Myanmar, Laos, and Thailand . This is also the point of confluence between the Ruak River (which follows the Thai–Myanmar border) and the Mekong. The area of this tripoint is sometimes termed the Golden Triangle , although the term also refers to the much larger area of those three countries that was notorious as a drug producing region. From the Golden Triangle tripoint, the Mekong turns southeast to briefly form

9588-592: The tumult of the Cultural Revolution . In the 1980s, students were trained in pinyin from an early age, learning it in tandem with characters or even before. During the height of the Cold War the use of pinyin system over Wade–Giles and Yale romanizations outside of China was regarded as a political statement or identification with the mainland Chinese government. Beginning in the early 1980s, Western publications addressing mainland China began using

9690-478: The underlying geological structure is fairly homogeneous and stable, exerting little or no control on river morphology . In marked contrast, the tributary networks of the Salween , Yangtze , and particularly the Mekong, are complex with different sub-basins often exhibiting different, and distinct, drainage patterns. These complex drainage systems have developed in a setting where the underlying geological structure

9792-634: The use and care of the Mekong. In 1996 China and Myanmar became "dialogue partners" of the MRC and the six countries now work together in a cooperative framework. In 2000, the governments of China, Laos, Thailand and Myanmar signed a Agreement on Commercial Navigation on Lancang-Mekong River among the Governments of the People's Republic of China, the Lao People's Democratic Republic, the Union of Myanmar and

9894-419: The vegetation does not. Shifting cultivation is common in the uplands of northern Laos and is reported to account for as much as 27% of the total land under rice cultivation. As elsewhere in the basin, forest cover has been steadily reduced during the last three decades by shifting agriculture and permanent agriculture. The cumulative impacts of these activities on the river regime have not been measured. However,

9996-464: The wars in Indochina in the 1970s, a significant quantity of explosives (sometimes, entire barges loaded with military ordnance ) sank in the Cambodian section of the Mekong (as well as in the country's other waterways). Besides being a danger for fishermen, unexploded ordnance also creates problems for bridge and irrigation systems construction. As of 2013, Cambodian volunteers are being trained, with

10098-481: Was constructed largely through fluvial and tidal processes. At this time the delta was advancing at a rate of 17 to 18 m (56 to 59 ft) per year. After 3.5 ka, however, the delta had built out beyond the embayment and became subject to wave action and marine currents. These deflected deposition south-eastwards in the direction of the Cà Mau Peninsula , which is one of the most recent features of

10200-509: Was developed in the 1950s by a group of Chinese linguists including Wang Li , Lu Zhiwei , Li Jinxi , Luo Changpei and Zhou Youguang , who has been called the "father of pinyin". They based their work in part on earlier romanization systems . The system was originally promulgated at the Fifth Session of the 1st National People's Congress in 1958, and has seen several rounds of revisions since. The International Organization for Standardization propagated Hanyu Pinyin as ISO 7098 in 1982, and

10302-542: Was that the Mekong had too many falls and rapids to ever be useful for navigation . The river's source was found by Pyotr Kuzmich Kozlov in 1900. From 1893, the French extended their control of the river into Laos, establishing French Indochina by the first decade of the 20th century. This lasted until the First and Second Indochina Wars expelled French from its former colony and defeated US-supported governments. During

10404-626: Was used in English-language publications outside China until 1979. In 1943, the US military tapped Yale University to develop another romanization system for Mandarin Chinese intended for pilots flying over China—much more than previous systems, the result appears very similar to modern Hanyu Pinyin. Hanyu Pinyin was designed by a group of mostly Chinese linguists, including Wang Li , Lu Zhiwei , Li Jinxi , Luo Changpei , as well as Zhou Youguang (1906–2017), an economist by trade, as part of

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