Ouroun | |
---|---|
Commune and town | |
Country | |
Region | Sikasso Region |
Cercle | Bougouni Cercle |
Population (1998) | |
• Total | 3,947 |
Time zone | UTC+0 (GMT) |
Ouroun is a small town and commune in the Cercle of Bougouni in the Sikasso Region of southern Mali. In 1998 the commune had a population of 3,947. [1]
The population composed mainly of three ethnic groups: Bambara, Malinkés and Fulani. Ouroun is naturally divided into two districts: Sokoundéni and Sokoumba. The first is located southeast of the city, while the second is slightly north to south. With a population almost three times larger than that of Sokoundeni, Sokoumba is also divided by its inhabitants in two parts: Kourou and Kodjou. The latter is more inhabited than the first. [2]
Ouroun has a tropical climate. In summer, there is less rainfall than in winter. According to the Köppen-Geiger climate classification, the climate is As. The average annual temperature in Ouroun is 27.1 °C. The rainfall here averages 1103 mm. [3]
The driest month is December, with 0 mm of rainfall. The greatest amount of precipitation occurs in August, with an average of 291 mm.
With an average temperature of 30.7 °C, April is the warmest month of the year in Ouroun. At the same time January is the coldest month with an average of 24.2 °C. The precipitation varies 291 mm between the driest and the wettest months. The difference between the lowest and the highest temperature is 6.5 °C.
The desert climate, is a climate in which there is an excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates hold little moisture and evaporate the little rainfall they receive. Covering 14.2% of earth's land area, hot deserts are the most common type of climate on earth after polar climate.
Tropical climate is one of the five major climate groups in the Köppen climate classification. Tropical climates are characterized by monthly average temperatures of 18 ℃ (64.4 ℉) or higher year-round and feature hot temperatures. Annual precipitation is often abundant in tropical climates, and shows a seasonal rhythm to varying degrees. There are normally only two seasons in tropical climates, a wet season and a dry season. The annual temperature range in tropical climates is normally very small. Sunlight is intense.
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by the German-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.
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Coordinates: 11°42′05″N7°55′11″W / 11.70139°N 7.91972°W
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