Baruunturuun District Баруунтуруун сум ᠪᠠᠷᠠᠭᠤᠨᠲᠤᠷᠤᠭᠤᠨᠰᠤᠮᠤ | |
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District | |
Coordinates: 49°39′30″N94°23′57″E / 49.65833°N 94.39917°E Coordinates: 49°39′30″N94°23′57″E / 49.65833°N 94.39917°E | |
Country | Mongolia |
Elevation [1] | 1,232 m (4,045 ft) |
Population (2008) | |
• Total | 2,810 |
Baruunturuun (Mongolian : Баруунтуруун) is a sum in Uvs Province of Mongolia.
The Mongolian languageMoŋɣol kele; in Mongolian Cyrillic: монгол хэл, mongol khel) is the official language of Mongolia and both the most widely-spoken and best-known member of the Mongolic language family. The number of speakers across all its dialects may be 5.2 million, including the vast majority of the residents of Mongolia and many of the Mongolian residents of the Inner Mongolia Autonomous Region. In Mongolia, the Khalkha dialect, written in Cyrillic, is predominant, while in Inner Mongolia, the language is dialectally more diverse and is written in the traditional Mongolian script. In the discussion of grammar to follow, the variety of Mongolian treated is Standard Khalkha Mongolian, but much of what is to be said is also valid for vernacular (spoken) Khalkha and for other Mongolian dialects, especially Chakhar.
Uvs is one of the 21 aimags (provinces) of Mongolia. It is located in the west of the country, 1,336 kilometres or 830 miles away from the national capital Ulaanbaatar. Its capital is Ulaangom which lies 936 metres or 3,070 feet above sea level.
It is the heartland of grain production in the province,[ citation needed ] and lies on the bank of the Turuun River. The sum is also one of the most populous areas in the province. MIAT Mongolian Airlines flew to Baruunturuun directly from Ulan Bator until 2005, but stopped due to a plane shortage. Although the Baruunturuun Airport is not operational at the moment, it is considered the secondary airport of the province.[ citation needed ]
The Turuun River is a river of western Mongolia. It flows through the sum of Baruunturuun in Uvs Province.
MIAT Mongolian Airlines is the Mongolian national airline, headquartered in the MIAT Building in Ulaanbaatar, the capital of Mongolia. The airline operates international scheduled services from its base at Chinggis Khaan International Airport near Ulaanbaatar.
Baruunturuun has a continental climate (Köppen climate classification Dwb) closely bordering on a subarctic climate (Köppen climate classification Dwc) with warm summers and bitterly cold winters even for Mongolia, owing to very strong altitudinal temperature inversions from drainage of cold air into the western valleys. [2] The average minimum temperature in January is −36.3 °C (−33.3 °F), and temperatures as low as −49.9 °C (−57.8 °F) have been recorded. Temperatures in summer can be hot; the maximum temperature recorded is 39.2 °C (102.6 °F). Much precipitation falls in the summer as rain, with some snow in the spring and autumn. Winters are quite dry, with only light snowfall.
Continental climates often have a significant annual variation in temperature. They tend to occur in the middle latitudes, where prevailing winds blow overland, and temperatures are not moderated by bodies of water such as oceans or seas. Continental climates occur mostly in the Northern Hemisphere, which has the kind of large landmasses required for this type of climate to develop. Most of northern and northeastern China, eastern and southeastern Europe, central and southeastern Canada, and the central and upper eastern United States have this type of climate.
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by the Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system.
The subarctic climate is a climate characterised by long, usually very cold winters, and short, cool to mild summers. It is found on large landmasses, away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N poleward of the humid continental climates. These climates represent Köppen climate classification Dfc, Dwc, Dsc, Dfd, Dwd and Dsd. In very small areas at high altitudes around the Mediterranean Basin, Iran, Kyrgyzstan, Tajikistan, Turkey, Alaska and other parts of the northwestern United States and Russian South-Eastern regions the climate is classified as Dsc with a dry summer climate, such as in Seneca, Oregon or Atlin, British Columbia.
Climate data for Baruunturuun | |||||||||||||
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Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high °C (°F) | 4.9 (40.8) | 1.4 (34.5) | 12.2 (54) | 27.2 (81) | 37.5 (99.5) | 34.7 (94.5) | 39.2 (102.6) | 35.0 (95) | 33.5 (92.3) | 23.9 (75) | 13.5 (56.3) | 13.0 (55.4) | 39.2 (102.6) |
Average high °C (°F) | −24.7 (−12.5) | −21.8 (−7.2) | −10.4 (13.3) | 5.1 (41.2) | 17.6 (63.7) | 23.0 (73.4) | 23.7 (74.7) | 22.3 (72.1) | 16.6 (61.9) | 6.1 (43) | −7.5 (18.5) | −20.8 (−5.4) | 2.4 (36.4) |
Daily mean °C (°F) | −31.4 (−24.5) | −28.3 (−18.9) | −18.4 (−1.1) | −1.6 (29.1) | 10.1 (50.2) | 15.9 (60.6) | 17.1 (62.8) | 15.3 (59.5) | 8.9 (48) | −0.7 (30.7) | −14.3 (6.3) | −26.6 (−15.9) | −4.5 (23.9) |
Average low °C (°F) | −36.3 (−33.3) | −35.0 (−31) | −24.7 (−12.5) | −7.5 (18.5) | 2.6 (36.7) | 8.2 (46.8) | 10.9 (51.6) | 8.8 (47.8) | 2.7 (36.9) | −6.3 (20.7) | −19.9 (−3.8) | −31.5 (−24.7) | −10.7 (12.8) |
Record low °C (°F) | −49.9 (−57.8) | −45.9 (−50.6) | −40.6 (−41.1) | −30.2 (−22.4) | −12.2 (10) | −8.6 (16.5) | 0.0 (32) | −4.8 (23.4) | −12.0 (10.4) | −25.8 (−14.4) | −37.9 (−36.2) | −47.1 (−52.8) | −49.9 (−57.8) |
Average precipitation mm (inches) | 3.8 (0.15) | 3.3 (0.13) | 6.0 (0.236) | 13.0 (0.512) | 16.6 (0.654) | 31.6 (1.244) | 54.2 (2.134) | 43.0 (1.693) | 24.5 (0.965) | 12.6 (0.496) | 9.0 (0.354) | 6.3 (0.248) | 223.9 (8.816) |
Average precipitation days (≥ 1.0 mm) | 1.4 | 1.3 | 1.9 | 3.4 | 2.8 | 5.8 | 7.8 | 7.1 | 4.1 | 3.2 | 2.7 | 1.9 | 43.4 |
Source: NOAA (1961-1990) [3] |
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A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by large seasonal temperature differences, with warm to hot summers and cold winters. Precipitation is usually distributed throughout the year. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below −3 °C (26.6 °F) and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition, the location in question must not be semi-arid or arid. The Dfb, Dwb and Dsb subtypes are also known as hemiboreal.
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