Baruunturuun
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Baruunturuun (Template:Langx) is a sum in Uvs Province of Mongolia.
It is the heartland of grain production in the province,Script error: No such module "Unsubst". 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 Ulaanbaatar 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.Script error: No such module "Unsubst".
Climate
Baruunturuun has a continental climate (Köppen climate classification Dwb, Trewartha climate classification Dcld) closely bordering on a subarctic climate (Köppen climate classification Dwc, Trewartha Ecld) with mild to 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.[1]
Baruunturuun experiences 209.9 days per year with minimum temperature below the freezing point and 151 days in which the maximum temperature is below such threshold.[2] The average minimum temperature in January is Script error: No such module "convert"., and the lowest recorded temperature was Script error: No such module "convert".. Temperatures in summer can be hot; in 10.9 days per year the daily maximum temperature is at or above Script error: No such module "convert"..[2] The highest temperature recorded is Script error: No such module "convert".. Much precipitation falls in the summer as rain, with some snow in the spring and autumn. Winters are quite dry, with only light snowfall. The average wind speed does not exceed Script error: No such module "convert". in winter.[2]
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Administrative divisions
The district is divided into four bags, which are:[3]
- Bayan-Airag
- Shand
- Turuun
- Zuun Turuun
References
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- ↑ Bayasgalan Gerelchuluun and Ahn Joong-Bae; ‘Air temperature distribution over Mongolia using dynamical downscaling and statistical correction’, International Journal of Climatology; 34:2464-2476 (2014)
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