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Climate Dynamics

, Volume 52, Issue 5–6, pp 3599–3608 | Cite as

Extremes in the magnitude of annual temperature cycle on the Tibetan Plateau over the past three centuries

  • Jianping DuanEmail author
  • Zhuguo Ma
  • Naiming Yuan
  • Lun Li
  • Liang Chen
Article

Abstract

Weakening of annual temperature cycle (ATC) on the Tibetan Plateau (TP) in the last decades has been identified, and there is a subsequent change in the frequency of the ATC magnitude extremes. These changes in the climate have a potential influence on biological and ecological systems. However, the frequency of occurrences of the ATC magnitude extremes in the recent decades compared to the preindustrial period, as well as the potential driving forces remains unclear. This can limit the robust predictions and risk assessments for extreme events of the ATC in the future. In this study, we analyzed the frequency of occurrence of the ATC magnitude extremes using both recent observations (1955–2011) and a tree-ring-based reconstruction covering the past three centuries over the TP. The results indicate that the ATC magnitude extremes in maximum obviously decrease and in minimum distinctly increase under climate warming, both for the instrumental period and the past three centuries. Moreover, the occurrence of the ATC magnitude extremes on the TP had a distinct regional characteristic and was mainly related to the winter temperature extremes triggered by the anomalous meridional gradient of geopotential height impelling cold air intrudes the TP. Although volcanic eruptions were expected to result in summer cooling and winter warming, and thus trigger the minimum ATC magnitude extremes, this effect only can be identified in event-specific eruptions (e.g., the 1835 Cosiguina eruption). Our study results provide an essential background for developing robust predictions and risk assessments for the ATC magnitude extremes on the TP.

Keywords

Tibetan Plateau Annual temperature cycle Extreme climate events Tree rings 

Notes

Acknowledgements

This research was supported by the National Key R&D Program of China (2016YFA0600404), the National Natural Science Foundation of China (Grants 41471035, 41101043 and 41405054). Climate data from the meteorological stations were obtained from the National Meteorological Information Center of China Meteorological Administration. Jianping Duan acknowledges support from the Alexander von Humboldt Foundation.

References

  1. Adams JB, Mann ME, Ammann CM (2003) Proxy evidence for an El Niño-like response to volcanic forcing. Nature 426:274–278CrossRefGoogle Scholar
  2. Deng Y, Gou XH, Gao LL, Yang T, Yang MX (2014) Early-summer temperature variations over the past 563 year inferred from tree rings in the Shaluli Mountains, southeastern Tibet Plateau. Quat Res 81:513–519CrossRefGoogle Scholar
  3. Dong B, Sutton RT, Shaffrey L (2017) Understanding the rapid summer warming and changes in temperature extremes since the mid-1990s over Western Europe. Clim Dyn 48:1537–1554CrossRefGoogle Scholar
  4. Duan JP, Zhang QB, Lv LX (2013) Increased variability in cold-season temperature since the 1930s in subtropical China. J Clim 26:4749–4757CrossRefGoogle Scholar
  5. Duan JP, Li L, Fang YJ (2015) Seasonal spatial heterogeneity of warming rates on the Tibetan Plateau over the past 30 years. Sci Rep 5:11725CrossRefGoogle Scholar
  6. Duan JP et al (2017) Weakening of annual temperature cycle over the Tibetan Plateau since the 1870s. Nat Commun 8:14008CrossRefGoogle Scholar
  7. Fan JW et al (2010) Assessment of effects of climate change and grazing activity on grassland yield in the three rivers headwaters region of Qinghai-Tibet Plateau, China. Environ Monit Assess 170:571–584CrossRefGoogle Scholar
  8. Fischer EM, Schär C (2010) Consistent geographical patterns of changes in high-impact European heatwaves. Nat Geosci 3:398–403CrossRefGoogle Scholar
  9. IPCC Climate Change (2013) (2013) The physical science basis. In: Contribution of working group I to the 5th assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge, p 72Google Scholar
  10. Jentsch A, Beierkuhnlein C (2008) Research frontiers in climate change: effects of extreme meteorological events on ecosystems. C R Geosci 340:621–628CrossRefGoogle Scholar
  11. Jones PD, Lister DH, Osborn TJ, Harpham C, Salmon M, Morice CP (2012) Hemispheric and large-scale land-surface air temperature variations: an extensive revision and an update to 2010. J Geophys Res Atmos 117:D05127Google Scholar
  12. Li ZS, Liu GH, Wu X, Wang XC (2015) Tree-ring-based temperature reconstruction for the Wolong Natural Reserve, western Sichuan Plateau of China. Int J Climatol 35:3296–3307CrossRefGoogle Scholar
  13. Liang EY, Shao XM, Qin NS (2008) Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau. Global Planet Change 61:313–320CrossRefGoogle Scholar
  14. Liu XD, Yin ZY, Shao XM, Qin NS (2006) Temporal trends and variability of daily maximum and minimum, extremetemperature events,andgrowingseason lengthoverthe eastern and central Tibetan Plateau during 1961–2003. J Geophys Res 111:D19109CrossRefGoogle Scholar
  15. Meehl G, Karl T, Easterling D, Changnon S, Pielke R, Changnon D, Evans J, Groisman P, Knutson T, Kunkel K, Mearns L, Parmesan C, Pulwarty R, Root T, Sylves R, Whetton P, Zwiers F (2000) An introduction to trends in extreme weather and climate events: observations, socioeconomic impacts, terrestrial ecological impacts and model projections. Bull Am Meteorol Soc 81:413–416CrossRefGoogle Scholar
  16. Qian C, Zhang XB (2015) Human influences on changes in the temperature seasonality in mid- to high-latitude land areas. J Clim 28:5908–5921CrossRefGoogle Scholar
  17. Ren G, Zhou Y (2014) Urbanization effect on trends of extreme temperature indices of national stations over mainland China, 1961–2008. J Clim 27:2340–2360CrossRefGoogle Scholar
  18. Robock A (2000) Volcanic eruptions and climate. Rev Geophys 38:191–219CrossRefGoogle Scholar
  19. Robock A, Mao J (1992) Winter warming from large volcanic eruptions. Geophys Res Lett 12:2405–2408CrossRefGoogle Scholar
  20. Shi SY, Li JB, Shi JF, Zhao YS, Huang G (2017) Three centuries of winter temperature change on the southeastern Tibetan Plateau and its relationship with the Atlantic Multidecadal Oscillation. Clim Dyn 49:1305–1319CrossRefGoogle Scholar
  21. Sigl M et al (2014) Insights from Antarctica on volcanic forcing during the common era. Nat Clim Change 4:693–697CrossRefGoogle Scholar
  22. Smith M (2011) An ecological perspective on extreme climatic events: a synthetic definition and framework to guide future research. J Ecol 99:656–663CrossRefGoogle Scholar
  23. Stine AR, Huybers P (2012) Changes in the seasonal cycle of temperature and atmospheric circulation. J Climate 25:7362–7380CrossRefGoogle Scholar
  24. Stott PA, Stone DA, Allen MR (2004) Human contribution to the European heatwave of 2003. Nature 432:610–644CrossRefGoogle Scholar
  25. Wallace CJ, Osborn TJ (2002) Recent and future modulation of the annual cycle. Clim Res 22:1–11CrossRefGoogle Scholar
  26. Wang G, Dillon ME (2014) Recent geographic convergence in diurnal and annual temperature cycling flattens global thermal profiles. Nat Clim Change 4:988–992CrossRefGoogle Scholar
  27. Wang JL et al (2014) Tree-ring inferred annual mean temperature variations on the southeastern Tibetan Plateau during the last millennium and their relationships with the Atlantic Multidecadal Oscillation. Clim Dyn 43:627–640CrossRefGoogle Scholar
  28. You QL et al (2008) Changes in daily climate extremes in the eastern and central Tibetan Plateau during 1961–2005. J Geophys Res Atmos 113:D07101CrossRefGoogle Scholar
  29. Zhai P, Pan XH (2003) Trends in temperature extremes during 1951–1999 in China, Geophys Res Lett 30: 1913Google Scholar
  30. Zhang Y, Shao XM, Yin ZY, Wang Y (2014) Millennial minimum temperature variations in the Qilian Mountains, China: evidence from tree rings. Clim Past 10:1763–1778CrossRefGoogle Scholar

Copyright information

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

Authors and Affiliations

  • Jianping Duan
    • 1
    Email author
  • Zhuguo Ma
    • 1
  • Naiming Yuan
    • 1
  • Lun Li
    • 2
  • Liang Chen
    • 1
  1. 1.CAS Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric PhysicsChinese Academy of SciencesBeijingChina
  2. 2.Chinese Academy of Meteorological SciencesBeijingChina

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