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Alexis Berg and Justin Sheffield

models. We also explore the potential relationships between the spread in ET partitioning and general aspects of the simulated climate in these models. Finally, we investigate what future changes in partitioning models simulate in response to anthropogenic forcing and global warming and what factors are driving these changes. 2. Data and methods We use monthly outputs from historical and representative concentration pathway 8.5 (RCP8.5; Riahi et al. 2011 ) simulations from the CMIP5 experiment. We

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Suzana J. Camargo, Claudia F. Giulivi, Adam H. Sobel, Allison A. Wing, Daehyun Kim, Yumin Moon, Jeffrey D. O. Strong, Anthony D. Del Genio, Maxwell Kelley, Hiroyuki Murakami, Kevin A. Reed, Enrico Scoccimarro, Gabriel A. Vecchi, Michael F. Wehner, Colin Zarzycki, and Ming Zhao

1. Introduction Since the 1970s climate models have been known to simulate tropical cyclone–like structures ( Manabe et al. 1970 ; Bengtsson et al. 1982 ; Haarsma et al. 1993 ). These models have been used for projections of tropical cyclone (TC) activity under anthropogenic climate change ( Broccoli and Manabe 1990 ; Bengtsson et al. 1996 ) and their use for such projections continues to this day, using low- ( Camargo 2013 ; Tory et al. 2013 ; Chand et al. 2017 ) and high

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