How do continental air masses affect temperatures in the Kunlun Mountains?

The Kunlun Mountains are almost entirely isolated from the climatic influence of the Indian and Pacific Ocean monsoons. Instead, the region remains under the constant influence of the continental air mass, which is the primary driver of the area's temperature patterns.1

This persistent exposure to continental air results in significant annual and diurnal (daily) temperature fluctuations. In the high-elevation zones, these sharp daily temperature shifts create intense weathering conditions caused by the cycle of heat and frost.1

The impact of these air masses varies by elevation:
* Lower mountain tiers: Average temperatures range from 77 to 82 °F (25 to 28 °C) in July and remain at or above 16 °F (−9 °C) in January.1
* Upper mountain tiers and the Tibetan border: Average July temperatures are below 50 °F (10 °C), while winter temperatures frequently drop to −31 °F (−35 °C) or lower.1