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Johna E. Rudzin, Lynn K. Shay, and Benjamin Jaimes de la Cruz

forcing, since entrainment cooling is less with deep-ocean mixed layers, and sustain air–sea fluxes into the storm ( Shay et al. 2000 ; Lin et al. 2005 , 2009 , 2013 ; Shay and Uhlhorn 2008 ; Jaimes and Shay 2009 , 2010 ; Jaimes et al . 2015 ). In addition to ocean thermal structure, a few studies have indicated that the upper-ocean salinity stratification within the Amazon–Orinoco River plume plays a role in modulating SST during TC passage by reducing the efficiency of upper-ocean mixing

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Kuan-Ting O, Robert Wood, and Christopher S. Bretherton

Celik , F. , and J. D. Marwitz , 1999 : Droplet spectra broadening by ripening process. Part I: Roles of curvature and salinity of cloud droplets . J. Atmos. Sci. , 56 , 3091 – 3105 , https://doi.org/10.1175/1520-0469(1999)056<3091:DSBBRP>2.0.CO;2 . 10.1175/1520-0469(1999)056<3091:DSBBRP>2.0.CO;2 Chen , J. , Y. Liu , M. Zhang , and Y. Peng , 2016 : New understanding and quantification of the regime dependence of aerosol-cloud interaction for studying aerosol indirect effects

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