Does the climate warming hiatus exist over the Tibetan Plateau?

Scientific Reports
Anmin Duan, Zhixiang Xiao

Abstract

The surface air temperature change over the Tibetan Plateau is determined based on historical observations from 1980 to 2013. In contrast to the cooling trend in the rest of China, and the global warming hiatus post-1990s, an accelerated warming trend has appeared over the Tibetan Plateau during 1998-2013 (0.25 °C decade(-1)), compared with that during 1980-1997 (0.21 °C decade(-1)). Further results indicate that, to some degree, such an accelerated warming trend might be attributable to cloud-radiation feedback. The increased nocturnal cloud over the northern Tibetan Plateau would warm the nighttime temperature via enhanced atmospheric back-radiation, while the decreased daytime cloud over the southern Tibetan Plateau would induce the daytime sunshine duration to increase, resulting in surface air temperature warming. Meanwhile, the in situ surface wind speed has recovered gradually since 1998, and thus the energy concentration cannot explain the accelerated warming trend over the Tibetan Plateau after the 1990s. It is suggested that cloud-radiation feedback may play an important role in modulating the recent accelerated warming trend over the Tibetan Plateau.

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Citations

Nov 15, 2017·Scientific Reports·Yuanyuan WangGuanghua Qin
Oct 12, 2019·Science·Jie PeiZheng Niu
Jul 2, 2017·Scientific Reports·Jieru MaYongkun Xie
Feb 13, 2021·The Science of the Total Environment·Guoqing ZhangJean-François Crétaux
Feb 2, 2021·Ecology and Evolution·Wen-Ting WangJens-Christian Svenning
Sep 17, 2021·Environmental Monitoring and Assessment·Jairam Singh YadavRavi K Yadav
Nov 11, 2021·The Science of the Total Environment·Arushi SharmaChandra Venkataraman

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