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Anne S. Daloz, S. J. Camargo, J. P. Kossin, K. Emanuel, M. Horn, J. A. Jonas, D. Kim, T. LaRow, Y.-K. Lim, C. M. Patricola, M. Roberts, E. Scoccimarro, D. Shaevitz, P. L. Vidale, H. Wang, M. Wehner, and M. Zhao

–dynamical downscaling technique described in Emanuel (2006) and Emanuel et al. (2006) . One benefit of this type of downscaling technique is to generate a very large number of synthetic storm tracks with realistic intensity based on climate model environmental fields. This technique has been successfully applied to various reanalyses ( Emanuel 2010 ) and climate models ( Emanuel et al. 2008 , 2010 ; Emanuel 2013 ) and coupled with storm surge models ( Lin et al. 2012 ). However, this technique also presents

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