Theoretical and Applied Climatology

, Volume 135, Issue 3–4, pp 1375–1385 | Cite as

Warming slowdown over the Tibetan plateau in recent decades

  • Yaojie Liu
  • Yangjian ZhangEmail author
  • Juntao Zhu
  • Ke Huang
  • Jiaxing Zu
  • Ning Chen
  • Nan Cong
  • Annemiek Irene Stegehuis
Original Paper


As the recent global warming hiatus and the warming on high elevations are attracting worldwide attention, this study examined the robustness of the warming slowdown over the Tibetan plateau (TP) and its related driving forces. By integrating multiple-source data from 1982 to 2015 and using trend analysis, we found that the mean temperature (Tmean), maximum temperature (Tmax) and minimum temperature (Tmin) showed a slowdown of the warming trend around 1998, during the period of the global warming hiatus. This was found over both the growing season (GS) and non-growing season (NGS) and suggested a robust warming hiatus over the TP. Due to the differences in trends of Tmax and Tmin, the trend of diurnal temperature range (DTR) also shifted after 1998, especially during the GS temperature. The warming rate was spatially heterogeneous. The northern TP (NTP) experienced more warming than the southern TP (STP) in all seasons from 1982 to 1998, while the pattern was reversed in the period from 1998 to 2015. Water vapour was found to be the main driving force for the trend in Tmean and Tmin by influencing downward long wave radiation. Sunshine duration was the main driving force behind the trend in Tmax and DTR through a change in downward shortwave radiation that altered the energy source of daytime temperature. Water vapour was the major driving force for temperature change over the NTP, while over the STP, sunshine duration dominated the temperature trend.


Tibetan plateau Warming hiatus Land surface temperature MODIS Mann-Kendall 



We thank Jian Tao, Tao Zhang, Yi Xi, Jyoti Bhandari, Ze Tang, Junxiang Li and Yixuan Zhu for their valuable comments and suggestions. We also thank the journal editor and the anonymous reviewers for their useful comments and efforts on this paper.


This research was funded by the following projects: the Chinese National Key Program for Developing Basic Science (2013CB956302) and the Science and Technology Project of the Chinese Academy of Sciences (XDA05050400).

Supplementary material

704_2018_2435_MOESM1_ESM.doc (366 kb)
ESM 1 (DOC 366 kb)


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Copyright information

© Springer-Verlag GmbH Austria, part of Springer Nature 2018

Authors and Affiliations

  • Yaojie Liu
    • 1
    • 2
  • Yangjian Zhang
    • 1
    • 2
    • 3
    Email author
  • Juntao Zhu
    • 1
  • Ke Huang
    • 1
    • 2
  • Jiaxing Zu
    • 1
    • 2
  • Ning Chen
    • 1
    • 2
  • Nan Cong
    • 1
  • Annemiek Irene Stegehuis
    • 4
  1. 1.Lhasa Plateau Ecosystem Research Station, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources ResearchChinese Academy of SciencesBeijingChina
  2. 2.College of Resources and EnvironmentUniversity of Chinese Academy of SciencesBeijingChina
  3. 3.Center for Excellence in Tibetan Plateau Earth SciencesChinese Academy of SciencesBeijingChina
  4. 4.Shenzhen Key Laboratory of Circular Economy, School of Urban Planning and Design, Shenzhen Graduate SchoolPeking UniversityShenzhenChina

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