Skip to main content

Advertisement

Log in

Potential regulation on the climatic effect of Tibetan Plateau heating by tropical air–sea coupling in regional models

  • Published:
Climate Dynamics Aims and scope Submit manuscript

Abstract

Based on the conventional weather research and forecasting (WRF) model and the air–sea coupled mode WRF-OMLM, we investigate the potential regulation on the climatic effect of Tibetan Plateau (TP) heating by the air–sea coupling over the tropical Indian Ocean and western Pacific. Results indicate that the TP heating significantly enhances the southwesterly monsoon circulation over the northern Indian Ocean and the South Asia subcontinent. The intensified southwesterly wind cools the sea surface mainly through the wind-evaporation-SST (sea surface temperature) feedback. Cold SST anomaly then weakens monsoon convective activity, especially that over the Bay of Bengal, and less water vapor is thus transported into the TP along its southern slope from the tropical oceans. As a result, summer precipitation decreases over the TP, which further weakens the TP local heat source. Finally, the changed TP heating continues to influence the summer monsoon precipitation and atmospheric circulation. To a certain extent, the air–sea coupling over the adjacent oceans may weaken the effect of TP heating on the mean climate in summer. It is also implied that considerations of air–sea interaction are necessary in future simulation studies of the TP heating effect.

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

Similar content being viewed by others

References

  • Abe M, Hori M, Yasunari T, Kitoh A (2013) Effects of the Tibetan Plateau on the onset of the summer monsoon in South Asia: the role of the air–sea interaction. J Geophys Res 118:1760 – 1776

    Article  Google Scholar 

  • Boos W, Kuang Z (2010) Dominant control of the South Asian monsoon by orographic insulation versus plateau heating. Nature 463:218–223

    Article  Google Scholar 

  • Duan A, Wu G (2005) Role of the Tibetan Plateau thermal forcing in the summer climate pattern over subtropical Asia. Clim Dyn 24:793–807

    Article  Google Scholar 

  • Duan A, Sui C, Wu G (2008) Simulation of local air–sea interaction in the great warm pool and its influence on Asian monsoon. J Geophys Res 113:D22105. https://doi.org/10.1029/2008JD010520

    Article  Google Scholar 

  • Duan A, Wu G, Liu Y, Ma Y, Zhao P (2012) Weather and climate effects of the Tibetan Plateau. Adv Atmos Sci 29:978–992

    Article  Google Scholar 

  • Gao Y, Xu J, Chen D (2015) Evaluation of WRF mesoscale climate simulations over the Tibetan Plateau during 1979–2011. J Clim 28(7):2823–2841

    Article  Google Scholar 

  • Gao Y, Xiao L, Chen D, Chen F, Xu J, Xu Y (2016) Quantification of the relative role of land-surface processes and large-scale forcing in dynamic downscaling over the Tibetan Plateau. Clim Dyn 48:1705–1721

    Article  Google Scholar 

  • He C, Zhou T, Wu B (2015) The key oceanic regions responsible for the interannual variability of the western north pacific subtropical high and associated mechanisms. J Meteorol Res 29(4):562–575

    Article  Google Scholar 

  • Hsu H, Liu X (2003) Relationship between the Tibetan Plateau heating and East Asian summer monsoon rainfall. Geophys Res Lett 30(20):2066. https://doi.org/10.1029/2003GL017909

    Article  Google Scholar 

  • Hu J, Duan A (2015) Relative contributions of the Tibetan Plateau thermal forcing and the Indian Ocean sea surface temperature basin mode to the interannual variability of the East Asian summer monsoon. Clim Dyn 45:2697–2711

    Article  Google Scholar 

  • Huffman G, Adler R, Bolvin D, Gu G, Nelkin E, Bowman K, Hong Y, Stocker E, Wolff D (2007) The TRMM multisatellite precipitation analysis: quasi-global, multi-year, combined-sensor precipitation estimates at fine scale. J Hydrometeorol 8:38–55

    Article  Google Scholar 

  • Jiang X, Li Y, Yang S, Yang K, Chen J (2016) Interannual variation of summer atmospheric heat source over the Tibetan Plateau and the role of convection around the western maritime continent. J Clim 29:121–138

    Article  Google Scholar 

  • Kitoh A (2004) Effects of mountain uplift on East Asian summer climate investigated by a coupled atmosphere–ocean GCM experiments. J Clim 17:783–802

    Article  Google Scholar 

  • Liu J, Wang Y, Wang A, Wang Y, Wang A, Hideaki O, Abbott RJ (2006) Radiation and diversification within the Ligularia–Cremanthodium–Parasenecio complex (Asteraceae) triggered by uplift of the Qinghai–Tibetan Plateau. Mol Phylogenet Evol 38:31–49

    Article  Google Scholar 

  • Liu Y, Hoskins B, Blackburn M (2007) Impact of Tibetan orography and heating on the summer flow over Asia. J Meteorol Soc Jpn 85B:1–19

    Article  Google Scholar 

  • Ma D, Boos W, Kuang Z (2014) Effects of orography and surface heat fluxes on the South Asian summer monsoon. J Clim 27:6647–6659

    Article  Google Scholar 

  • Manda A, Hirose N, Yanagi T (2005) Feasible method for the assimilation of satellite-derived SST with an ocean circulation model. J Atmos Ocean Technol 22:746–756

    Article  Google Scholar 

  • Noh Y, Kim H-J (1999) Simulations of temperature and turbulence structure of the oceanic boundary layer with the improved near surface process. J Geophys Res 104:15621–15634

    Article  Google Scholar 

  • Okajima H, Xie S-P (2007) Orographic effects on the northwestern Pacific monsoon: Role of air–sea interaction. Geophys Res Lett 34:L21708. https://doi.org/10.1029/2007GL032206

    Article  Google Scholar 

  • Rajagopalan B, Molnar P (2013) Signatures of Tibetan Plateau heating on Indian summer monsoon rainfall variability. J Geophys Res 118:1170–1178

    Google Scholar 

  • Reynolds R, Smith T, Liu C, Chelton D, Casey K, Schlax M (2007) Daily high-resolution-blended analyses for sea surface temperature. J Clim 20:5473–5496

    Article  Google Scholar 

  • Shukla R, Huang B (2016) Interannual variability of the Indian summer monsoon associated with the air–sea feedback in the northern Indian Ocean. Clim Dyn 46:1977–1990

    Article  Google Scholar 

  • Skamarock W, Klemp J, Dudhia J, Gill D, Barker D, Duda M, Huang X, Wang W (2008) A description of the advanced research WRF version 3. NCAR Technical Note NCAR/TN-475 + STR. https://doi.org/10.5065/D68S4MVH

  • Wang Z, Duan A (2012) A new ocean mixed-layer model coupled into WRF. Atmos Ocean Sci Lett 5:170–175

    Article  Google Scholar 

  • Wang Z, Duan A, Wu G (2014a) Impacts of boundary layer parameterization schemes and air–sea coupling on WRF simulation of the East Asian summer monsoon. Sci China Earth Sci 57:1–14

    Google Scholar 

  • Wang Z, Duan A, Wu G (2014b) Time-lagged impact of spring sensible heat over the Tibetan Plateau on the summer rainfall anomaly in East China: case studies using the WRF model. Clim Dyn 42:2885–2898

    Article  Google Scholar 

  • Wang Z, Duan A, Li M, He B (2016a) Influences of thermal forcing over the slope/platform of the Tibetan Plateau on Asian summer monsoon: numerical studies with WRF model. Chin J Geophys 59(5):474–487

    Article  Google Scholar 

  • Wang Z, Duan A, Wu G, Yang S (2016b) Mechanism for occurrence of precipitation over the southern slope of the Tibetan Plateau without local surface heating. Int J Climatol 36:4164–4171

    Article  Google Scholar 

  • Wu G, Zhang Y (1998) Tibetan Plateau forcing and the timing of the monsoon onset over South Asia and the South China Sea. Mon Weather Rev 126:913–927

    Article  Google Scholar 

  • Wu G, Liu Y, Wang T, Wan R, Liu X, Li W, Wang Z, Zhang Q, Duan A, Liang X (2007) The influence of the mechanical and thermal forcing of the tibetan plateau on the Asian climate. J Hydrometeorol 8:770–789

    Article  Google Scholar 

  • Wu G, Liu Y, He B, Bao Q, Duan A, Jin F (2012) Thermal controls on the Asian summer monsoon. Sci Rep 2:404

    Article  Google Scholar 

  • Wu G, Zhuo H, Wang Z, Liu Y (2016) Two types of summertime heating over the Asian large-scale orography and excitation of potential-vorticity forcing I. over the Tibetan Plateau. Sci China Earth Sci 59:1996–2008

    Article  Google Scholar 

  • Wu Y, Li Y, Jiang X, Dong Y (2017) Parameters sensitivity analysis on simulation of rainfall in drought-flood year on Qinghai-Tibetan Plateau by WRF model (in Chinese). Plat Meteorol 36:619–631

    Google Scholar 

  • Yanai M, Wu G (2006) In: Wang B (ed) Effects of the Tibetan Plateau, the Asian monsoon. Springer Praxis, New York, pp 513–549

    Google Scholar 

  • Ye D, Gao Y (1979) Tibetan Plateau meteorology (in Chinese). Science Press, Beijing

    Google Scholar 

Download references

Acknowledgements

We are grateful to the anonymous reviewers who provided thoughtful comments and valuable suggestions on this paper. This work was supported jointly by the National Natural Science Foundation of China (Grants 41605038 and 91637208), the Natural Science Foundation of Guangdong Province (Grant 2015A030310224), and the Zhuhai Joint Innovative Center for Climate, Environment and Ecosystem.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Ziqian Wang.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Wang, Z., Duan, A. & Yang, S. Potential regulation on the climatic effect of Tibetan Plateau heating by tropical air–sea coupling in regional models. Clim Dyn 52, 1685–1694 (2019). https://doi.org/10.1007/s00382-018-4218-z

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00382-018-4218-z

Keywords

Navigation