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Volume 17, issue 22 | Copyright
Atmos. Chem. Phys., 17, 13731-13745, 2017
https://doi.org/10.5194/acp-17-13731-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 17 Nov 2017

Research article | 17 Nov 2017

Direct radiative effects of dust aerosols emitted from the Tibetan Plateau on the East Asian summer monsoon – a regional climate model simulation

Hui Sun et al.
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Alfaro, S. C. and Gomes, L.: Modeling mineral aerosol production by wind erosion: emission intensities and aerosol size distributions in source areas, J. Geophys. Res., 106, 18075–18084, https://doi.org/10.1029/2000JD900339, 2001.
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Bibi, H., Alam, K., Chishtie, F., Bibi, S., Shahid, I., and Blaschke, T.: Intercomparison of MODIS, MISR, OMI, and CALIPSO aerosol optical depth retrievals for four locations on the Indo-Gangetic plains and validation against AERONET data, Atmos. Environ., 111, 113–126, 2015.
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This study simulated the distribution of dust aerosols originating within the Tibetan Plateau (TP) and their radiative effects on the East Asian summer monsoon (EASM). The results showed that direct radiative cooling in the mid-troposphere induced by the TP locally produced dust aerosols resulted in the weakening of the EASM. Although contribution to the total Asian dust source from within TP is relatively small, its impacts on Asian monsoon and climate seems disproportionately large.
This study simulated the distribution of dust aerosols originating within the Tibetan Plateau...
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