Gobi Desert it is also located on a plateau roughly above sea level, which contributes to its low temperatures. An average of approximately of rain falls annually in the Gobi. Additional moisture reaches parts of the Gobi in winter as snow is blown by the wind from the Siberian Steppes. These winds may cause the Gobi to reach in winter to in summer. However, the climate of the Gobi is one of great extremes, combined with rapid changes of temperature of as much as . These can occur not only seasonally but within 24 hours. In southern Mongolia, the temperature has been
Gobi Desert Tuge-tau, its altitude being above the level of the sea and some above the crown of the swelling itself. This range he considers to belong to the Choltagh system, whereas Sven Hedin would assign it to the Kuruk-tagh. This last, which is pretty certainly identical with the range of Kharateken-ula (also known as the Kyzyl-sanghir, Sinir, and Singher Mountains), that overlooks the southern shore of the Lake Bosten, though parted from it by the drift-sand desert of Ak-bel-kum (White Pass Sands), has at first a west-northwest to east-southeast strike, but it gradually curves round like a scimitar towards the east-northeast