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James N. Moum, Simon P. de Szoeke, William D. Smyth, James B. Edson, H. Langley DeWitt, Aurélie J. Moulin, Elizabeth J. Thompson, Christopher J. Zappa, Steven A. Rutledge, Richard H. Johnson, and Christopher W. Fairall

thickness while reducing the total aerosol number and thus potential CCN concentrations ( Fig. SB2 ). As demonstrated from these in situ aerosol measurements taken during the November MJO event, MJO-related convection had a significant effect on relative concentrations of submicron continental and marine aerosol and supermicron primary marine aerosol over the Indian Ocean ( DeWitt et al. 2013 ). Changing aerosols translate into regional changes of the aerosol optical thicknesses and concentrations of

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