Abstract
Regional Atmospheric Modeling System (RAMS) was applied to the study of the effect of the topographical altitude of the Tibetan Plateau (TP) on a severe drought event which took place in eastern China from November 2008 to January 2009. Two simulations of this drought event were conducted: a control simulation (CNTRL run) using original model settings and a sensitive simulation (TOPO run), where no change other than to reduce the TP topography by 50 %. The results show that the CNTRL simulation validates RAMS by reproducing this drought event fairly accurately. However, as part of the TOPO simulation, the total heat flux showed a decrease over most parts of the TP, latent heat flux underwent a significant increase over the southeastern TP, contrary to sensible heat, and a universal decrease over eastern China; this led to an increase in precipitation over the southeastern TP and a decrease in precipitation over eastern China. The decrease of total heat flux over the TP is collocated with an anomalous anticyclonic circulation from the TP to the coasts of southeastern China. Changes in atmospheric circulation and low-level water vapor transport pathways were consistent with changes in precipitation. In general, reducing the topographical altitude of the TP worsens drought in eastern China and moreover causes a significant decrease in precipitation over southern China.
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Acknowledgments
This work was supported by the Chinese Academy of Sciences (Grant No. XDB03030201), the National Natural Science Foundation of China (Grant Nos. 91337212, 41275010, and 41375009), the External Cooperation Program of the Chinese Academy of Sciences (Grant No. GJHZ1207), the CMA Special Fund for Scientific Research in the Public Interest (Grant No. GYHY201406001), the EU-FP7 “CORE-CLIMAX” Projects (Grant No. 313085), and CAS “Hundred Talent” program (Dr. Weiqiang Ma). The authors are grateful to the anonymous reviewers for their valuable comments and suggestions.
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Meng, C., Ma, Y., Han, C. et al. Effect of reducing the topographical altitude of the Tibetan Plateau on a severe winter drought in eastern China as determined using RAMS. Theor Appl Climatol 129, 891–900 (2017). https://doi.org/10.1007/s00704-016-1817-7
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DOI: https://doi.org/10.1007/s00704-016-1817-7