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Zhining Tao, Scott A. Braun, Jainn J. Shi, Mian Chin, Dongchul Kim, Toshihisa Matsui, and Christa D. Peters-Lidard

precipitation from shallow clouds but invigorate deep convective rain clouds with warm cloud bases. Shi et al. (2014) investigated the impacts of the aerosol indirect and direct effects on the mesoscale convective system (MCS) over the West Africa region and found that the dust aerosol indirect effect was overwhelmed by their direct effect, which delayed the onset of the MCS. Based on an observational investigation of a trans-Atlantic Saharan dust outbreak event in March 2004, Min et al. (2009

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E. P. Nowottnick, P. R. Colarco, S. A. Braun, D. O. Barahona, A. da Silva, D. L. Hlavka, M. J. McGill, and J. R. Spackman

and Data Assimilation, 92 pp. Rosenfeld , D. , Y. Rudich , and R. Lahav , 2001 : Desert dust suppressing precipitation: A possible desertification feedback loop . Proc. Natl. Acad. Sci. USA , 98 , 5975 – 5980 , . 10.1073/pnas.101122798 Rotstayn , L. D. , 1999 : Indirect forcing by anthropogenic aerosols: A global climate model calculation of the effective‐radius and cloud‐lifetime effects . J. Geophys. Res. , 104 , 9369 – 9380 , https

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