Ömnögovi District Өмнөговь сум ᠡᠮᠦᠨᠡᠭᠣᠪᠢᠰᠤᠮᠤ | |
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District | |
Coordinates: 49°6′23″N91°43′7″E / 49.10639°N 91.71861°E Coordinates: 49°6′23″N91°43′7″E / 49.10639°N 91.71861°E | |
Country | Mongolia |
Province | Uvs Province |
Time zone | UTC + 7 (UTC+7) |
Ömnögovi (Mongolian : Өмнөговь, translit. Ömnögowĭ) is a sum (district) of Uvs Province in western 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.
Part of the sum is desert, that has sand dunes.
Ömnögovi has a semi-arid climate (Köppen climate classification BSk) with warm summers and severely cold winters. The average minimum temperature in January is −28.3 °C (−18.9 °F), and temperatures as low as −45.5 °C (−49.9 °F) have been recorded. Most precipitation falls in the summer as rain, with some snow in the adjacent months of May and September. Winters are very dry.
A semi-arid climate or steppe climate is the climate of a region that receives precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes.
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.
Climate data for Ömnögovi | |||||||||||||
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Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high °C (°F) | 3.2 (37.8) | 8.2 (46.8) | 17.5 (63.5) | 24.3 (75.7) | 28.3 (82.9) | 31.3 (88.3) | 33.6 (92.5) | 38.9 (102) | 29.7 (85.5) | 24.4 (75.9) | 11.9 (53.4) | 9.2 (48.6) | 38.9 (102) |
Average high °C (°F) | −15.2 (4.6) | −11.1 (12) | −0.4 (31.3) | 8.6 (47.5) | 16.7 (62.1) | 21.6 (70.9) | 22.5 (72.5) | 21.0 (69.8) | 15.3 (59.5) | 6.9 (44.4) | −3.8 (25.2) | −13.1 (8.4) | 5.8 (42.3) |
Daily mean °C (°F) | −22.6 (−8.7) | −19.5 (−3.1) | −8.6 (16.5) | 1.0 (33.8) | 9.5 (49.1) | 15.0 (59) | 16.2 (61.2) | 14.2 (57.6) | 7.9 (46.2) | −0.6 (30.9) | −10.9 (12.4) | −20.3 (−4.5) | −1.6 (29.2) |
Average low °C (°F) | −28.4 (−19.1) | −26.0 (−14.8) | −16.0 (3.2) | −6.1 (21) | 2.2 (36) | 8.2 (46.8) | 10.5 (50.9) | 8.2 (46.8) | 1.2 (34.2) | −6.3 (20.7) | −16.4 (2.5) | −25.1 (−13.2) | −7.8 (17.9) |
Record low °C (°F) | −45.5 (−49.9) | −42.3 (−44.1) | −35.6 (−32.1) | −23.1 (−9.6) | −16.9 (1.6) | −3.0 (26.6) | 1.5 (34.7) | −1.8 (28.8) | −18.5 (−1.3) | −22.0 (−7.6) | −31.8 (−25.2) | −42.8 (−45) | −45.5 (−49.9) |
Average precipitation mm (inches) | 0.7 (0.028) | 0.5 (0.02) | 1.9 (0.075) | 4.3 (0.169) | 6.8 (0.268) | 24.9 (0.98) | 44.6 (1.756) | 27.0 (1.063) | 12.2 (0.48) | 3.0 (0.118) | 1.3 (0.051) | 1.4 (0.055) | 128.6 (5.063) |
Average precipitation days (≥ 1.0 mm) | 0.1 | 0.3 | 0.6 | 1.0 | 1.6 | 4.3 | 4.2 | 4.5 | 2.1 | 0.5 | 0.3 | 0.5 | 20 |
Source: NOAA (1963-1990) [1] |
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.
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