Articles | Volume 20, issue 20
https://doi.org/10.5194/acp-20-11823-2020
https://doi.org/10.5194/acp-20-11823-2020
Research article
 | 
21 Oct 2020
Research article |  | 21 Oct 2020

Distinct responses of Asian summer monsoon to black carbon aerosols and greenhouse gases

Xiaoning Xie, Gunnar Myhre, Xiaodong Liu, Xinzhou Li, Zhengguo Shi, Hongli Wang, Alf Kirkevåg, Jean-Francois Lamarque, Drew Shindell, Toshihiko Takemura, and Yangang Liu

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Cited articles

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Chiang, J. C. H., Fung, I. Y., Wu, C. H., Cai, Y. H., Edman, J. P., Liu, Y. W., Day, J. A., Bhattacharya, T., Mondal, Y., and Labrousse, C. A.: Role of seasonal transitions and westerly jets in East Asian paleoclimate, Quaternary Sci. Rev., 108, 111–129, https://doi.org/10.1016/j.quascirev.2014.11.009, 2015. 
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Chung, C. and Ramanathan, V.: Weakening of N. Indian SST gradients and the monsoon rainfall in India and the Sahel, J. Climate, 19, 2036–2045, 2006. 
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Short summary
Black carbon (BC) and greenhouse gases (GHGs) enhance precipitation minus evaporation (P–E) of Asian summer monsoon (ASM). Further analysis reveals distinct mechanisms controlling BC- and GHG-induced ASM P–E increases. The change in ASM P–E by BC is dominated by the dynamic effect of enhanced large-scale monsoon circulation, the GHG-induced change by the thermodynamic effect of increasing atmospheric water vapor. This results from different atmospheric temperature feedbacks due to BC and GHGs.
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