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intensity using AIRS/Aqua data, Geophys. Res. Lett., 36, L09809, doi:10.1029/2009GL037634. Sun, Donglian, W. K. M. Lau, Menas Kafatos, Zafer Boybeyi, Gregory Leptoukh, Chaiwei Yang, Ruixin Yang, 2009, Numerical Simulations of the Impacts of the Saharan Air on Atlantic Tropical Cyclone Development, J. Climate, 22, 6230–6250, doi: Tompkins, A. M. (2001), Organization of tropical convection in low vertical wind shears:The role of coldpools, J. Atmos. Sci., 58, 1650– 1672. Trenberth, K. E. (1991), Climate diagnostics from global analyses: Conservation of mass in ECMWF analyses, J. Clim., 4, 707–722. Tuleya, R. E., and Y. Kurihara (1981), A numerical study on the effects of environmental flow on tropical storm genesis, Mon. Wea. Rev, 109, 2487–2506. Twohy, C. H., et al. (2009), Saharan dust particles nucleate droplets in eastern Atlantic clouds, Geophys. Res. Lett., 36, L01807, doi:10.1029/2008GL035846 TWOMEY, S. A., PIEPGRASS, M. and WOLFE, T. L. (1984), An assessment of the impact of pollution on global cloud albedo, Tellus B, 36B, 356–366. doi: Wang, C. (2005), A modeling study of the response of tropical deep convection to the increase of cloud condensation nuclei concentration: 1. Dynamics and microphysics, J. Geophys. Res., 110, D21211, doi:. Wang, Y. (2009), How do outer spiral rainbands affect tropical cyclone structure and intensity? J. Atmos. Sci., 66, 1250–1273. Wong, M. M., and J. L. Chan (2004), Tropical Cyclone Intensity in Vertical Wind
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