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The Tibetan Plateau, [a] ... Here the average altitude exceeds 5,000 metres (16,000 ft) and winter temperatures can drop to −40 °C (−40 °F). As a result of this ...
Despite its large size and mountainous nature, variation of climate across the Tibetan Plateau is more steady than abrupt. The "river region" has a subtropical highland climate with moderate summer rainfall averaging around 500 millimetres (20 in) per year, and daytime temperatures ranging from around 7 °C (45 °F) in winter to 24 °C (75 °F ...
West Tibetan India • China: 1985 ... Stretching for 86 km, the temperature ranges from -10 °C to -20 °C. Oxygen level is 50% less than normal range. [14] Thorong ...
The Tibet Autonomous Region is located on the Tibetan Plateau, the highest region on Earth. In northern Tibet elevations reach an average of over 4,572 metres (15,000 ...
The Changtang Nature Reserve Map including part of the Changtang (labeled as CHANG-THANG) (DMA, 1975). Most of the Tibetan Changtang is now protected nature reserves consisting of the Chang Tang Nature Reserve, the second-largest nature reserve in the world, and four new adjoining smaller reserves totaling 496,000 square kilometres (192,000 sq mi) of connected nature reserves that represent an ...
Even so, the hottest temperatures nationwide are recorded in the Turpan Depression, where the climate is much drier and temperatures often exceed 40 °C (104 °F). [11] [12] Permafrost can be found at high elevations in the Tibetan Plateau and the Tian Shan mountains, [13] [14] as well as other mountainous areas in Northern China. [14]
The Tibetan Plateau is composed of three main regions, based on yearly precipitation levels and types of vegetation, namely the alpine meadow, alpine steppe, and the alpine desert-steppe. Since the Holocene, studies of fossil pollen records have shown that the alpine meadow has extended into areas that were previously alpine steppe as ...
This is known as an adiabatic process, which has a characteristic pressure-temperature curve. As the pressure gets lower, the temperature decreases. The rate of decrease of temperature with elevation is known as the adiabatic lapse rate, which is approximately 9.8 °C per kilometer (or 5.4 °F per 1000 feet) of altitude. [6]