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Page 5 - திபெத்தியன் பீடபூமி ஆராய்ச்சி News Today : Breaking News, Live Updates & Top Stories | Vimarsana

New permafrost thermal stability map better describes the permafrost on the Tibetan Plateau

Credit: @Science China Press The Tibetan Plateau (TP), which is also called Earth s Third Pole , is the highest and most extensive plateau in the world. TP is well known as the Asian water tower , where is the largest permafrost region among middle- and low-latitude regions in the world. The average temperature of permafrost on the TP is approximately -2?, this warm permafrost is more sensitive to climate change and human disturbance than that in Arctic. However, the degradation of permafrost may affect the stability of Asian water tower . Mapping the permafrost on the TP is therefore of critical importance. Due to the harsh natural environment, the ground measurement data such as mean annual ground temperature (MAGT) at a depth of zero annual amplitude (10-25 m) in permafrost area of TP is very limited, which leads to the large uncertainty of permafrost map in this area. With the accumulation of ground observation data and remote sensing big data, it is possible to mapping the

Chinese researchers recalibrate elevation history of Qinghai-Tibet Plateau

1 2020-12-13 21:05:59Xinhua Editor : Cheng Zizhuo ECNS App Download How did the Qinghai-Tibet Plateau grow to the top of the world? A new study led by Chinese researchers has found evidence to suggest the plateau rose to its current height more recently than previously thought. According to the study published online earlier this week in the journal Science Advances, the central and southern Qinghai-Tibet Plateau rose to between 3,500 meters and 4,500 meters around 26 million to 21 million years ago. The findings challenge the widely held belief that the plateau reached a height of 4,600 meters as early as 40 million years ago. Lead researcher Fang Xiaomin, from the Institute of Tibetan Plateau Research under the Chinese Academy of Sciences, said the results came from an analysis of fossil soils at the Lunpola Basin, a prime location for determining the elevation history of the plateau.

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