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 steeply, and its foot is fringed by a string of deep depressions, ranging from Lukchun ( below sea level) to Hami ( above sea-level). To the south of the Kuruk-tagh lie the desert of Lop Nur, the Kum-tagh desert, and the valley of the Bulunzir-gol. To this great swelling, which arches up between the two border-ranges of the Chol-tagh and Kuruk-tagh, the Mongols give the name of "Ghashuun-Gobi" or "Salt Desert". It is some across from north to south, and is traversed by a number of minor parallel ranges, ridges and chains of hills. Down its middle runs a broad