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

radiative transfer model, Carlson and Benjamin (1980) reported a 1 K day −1 warming averaged between 1000 and 500 hPa (including the air within and below the SAL) over the ocean due to dust. Karyampudi and Carlson (1988) claimed that radiative heating by dust was responsible for maintaining a warmer and deeper SAL over the ocean and enhancing the AEJ strength. Chen et al. (2010) examined the dust–radiation effect on the SAL over the eastern Atlantic using a regional model with interactive dust

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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

physics lidar: Instrument description and initial measurement results . Appl. Opt. , 41 , 3725 – 3734 , https://doi.org/10.1364/AO.41.003725 . 10.1364/AO.41.003725 Meng , Z. , P. Yang , G. W. Kattawar , L. Bi , K. N. Liou , and I. Laszlo , 2010 : Single-scattering properties of tri-axial ellipsoidal mineral dust aerosols: A database for application to radiative transfer calculations . J. Aerosol Sci. , 41 , 501 – 512 , https://doi.org/10.1016/j.jaerosci.2010.02.008 . 10

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