“It is critically important to understand what is happening as a result of global warming at high elevations on the plateau where nearly all of the current snow and ice in the region exists. Changes in these mountain snow reserves are critical for the supply of water to billions of people in both China and India, and they are threatened by climate change,” said Dr. Nick Pepin, lead author of the study.
Earlier research indicated that the rate of warming can be amplified with elevation, such that high-altitude environments often experience more rapid changes in temperature than lower ones. This phenomenon, known as Elevation-Dependent Warming (EDW), drove the scientists to explore temperature trends at high elevations across the Tibetan Plateau, where temperature readings are scarce yet crucial for understanding global warming.
Direct measurements of air temperature are unavailable in remote higher elevation regions, since harsh conditions often prohibit setting up manned weather stations. Scientists have to rely on satellites for information in higher elevation regions.
The raw satellite data, though potentially useful, is not representative enough for temperature trend analysis since clouds potentially confuse the data. Also, local factors such as vegetation and concrete/grasses can obscure the wider picture.
This is where the team’s research came in. They made a customized model so that precise air temperatures in Tibetan mountains could be deduced from satellite data.
With this model, the researchers found a marked peak in warming rates around 5000-5500 m in the Nyenchen Tanglha Mountains, one of the major ranges in the central part of the plateau. This warming is particularly strong during the day. The disappearance of snow cover seems to be the most obvious reason for this increased warming.
“Snow reflects sunlight during the day. So when it is reduced it causes even more warming, especially at the height where it is disappearing fastest,” said Dr. Pepin. During the night there is also enhanced warming more broadly at higher altitudes (up to 6500 m), which is thought to be related to changes in both cloud patterns and moisture.
Warming rates for daytime (top) and nighttime (bottom) derived from satellite data for the Nyenchen Tanglha Mountains over the last two decades. The figure on the left scale refers to median elevation, e.g., 5250 = 5000-5500 meters above sea-level. (Image by Dr. Pepin)
Dr. Pepin was supported by a PIFI scholarship provided by the Chinese Academy of Sciences and was hosted by the Institute of Tibetan Plateau Research. This study was supported by the Strategic Priority Research Program (PAN-TPE) of the Chinese Academy of Sciences.
