Skip to main content

Advertisement

Log in

Anthropogenic Contribution to the Rapid Warming over the Tibetan Plateau

  • Published:
Climate Dynamics Aims and scope Submit manuscript

Abstract

The Tibetan Plateau (TP) is rapidly warming, posing potential risks to regional to global climate and ecosystems. However, it remains ambiguous to what extent anthropogenic forcing contributes to the rapid TP warming based on observation. It is also unclear for the quantitative analysis of the anthropogenic effects on the dynamic and thermodynamic warming of the TP. Here we disentangle this issue using CN05.1 observations and a probability statistics model based on long term memory. The findings demonstrate that the anthropogenically-driven trend accelerates regional warming and is dominant for the rapid TP warming. The anthropogenically-driven warming was more than 1.2 °C in the central-western TP from 1980 to 2018, with anthropogenic contribution reaching up to ~ 60% for the observed warming (1.8–2.0 °C). Furthermore, we extract the dynamic and thermodynamic warming from the observed TP warming by dynamical adjustment method and determine the anthropogenic effect of each. The results show that anthropogenic contribution of thermodynamic warming exceeds 50% in most parts of TP, with over 70% in the southwest. The thermal effect is the main way of anthropogenic impact on the rapid TP warming.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8

Similar content being viewed by others

Data availability

The CN05.1 data are available from http://www.geophy.cn/CN/10.6038/cjg20130406. The monthly mean sea level pressure data are from the National Centers for Environmental Prediction/Department of Energy Atmospheric Model Inter-comparison Project reanalysis (https://psl.noaa.gov/data/gridded/data.ncep.reanalysis2.html).

References

Download references

Acknowledgements

We thank the supports of the National Natural Science Foundation of China (42130610, 41875096), the National Key Research and Development Program of China (2017YFC1502303), and the National Natural Science Foundation of China (41875083, 41905060, 41975091).

Funding

This work was supported by the National Natural Science Foundation of China (42130610, 41875096), the National Key Research and Development Program of China (2017YFC1502303), and the National Natural Science Foundation of China (41875083, 41905060, 41975091).

Author information

Authors and Affiliations

Authors

Contributions

YW, PY and GF conceived the study. YW collected the data, performed the data analysis, made the plots, and prepared the manuscript. FJ, BH and PF provided comments and suggestions regarding the manuscript. All authors read and approved the final manuscript.

Corresponding author

Correspondence to Guolin Feng.

Ethics declarations

Conflict of interest

The authors have no relevant financial or non-financial interests to disclose.

Additional information

Publisher's Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Wang, Y., Yan, P., Ji, F. et al. Anthropogenic Contribution to the Rapid Warming over the Tibetan Plateau. Clim Dyn 61, 329–339 (2023). https://doi.org/10.1007/s00382-022-06576-8

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00382-022-06576-8

Keywords

Navigation