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The Climate is extremely "continental". Temperatures in the Gobi can fall to −40 °C (−40 °F) in winter and rise to +40 °C (104 °F) in the summer. With an average yearly rainfall of about 100 mm (3.9 in), the climate is extremely arid. [1]
Bronze Age herder burials have been found in the Gobi desert, as well as Karasuk bronze knives, and Mongolian deer stones. [21] Between 5000 cal BP and 4500 cal BP there was a period of desertification. [21] [22] Due to the increasing aridity between 3500 cal BP and 3000 cal BP there was a decline in human habitation in the Gobi desert.
The reserve was established in 1975 and declared an International Biosphere Reserve in 1991. It comprises about 9000 km 2 of desert steppe, arid mountains, deserts and semi deserts. Temperatures can fall to -40 °C in winter and rise to +40 °C in the summer. Average snow cover lasts 97 days per year.
In hot deserts, the temperature during daytime can exceed 45 °C (113 °F) in summer and plunge below freezing point at night during winter. [48] One square centimeter (0.16 sq in) of windblown sand from the Gobi Desert. Such large temperature variations have a destructive effect on the exposed rocky surfaces.
Many deserts, such as the Sahara, are hot year-round, but others, such as East Asia's Gobi Desert, become quite cold during the winter. [1] Temperature extremes are a characteristic of most deserts. High daytime temperatures give way to cold nights because there is no insulation provided by humidity and cloud cover. The diversity of climatic ...
The Best Temperature When You Are Home. During the winter, figuring out the best temperature while you're at home may not be so straightforward.
A major environmental issue in China is the continued expansion of its deserts, particularly the Gobi Desert. [ 57 ] [ 58 ] Although barrier tree lines planted since the 1970s have reduced the frequency of sandstorms , prolonged drought and poor agricultural practices have resulted in dust storms plaguing northern China each spring, which then ...
The desert climate or arid climate (in the Köppen climate classification BWh and BWk) is a dry climate sub-type in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive.
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