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Kyle A. Hilburn, Imme Ebert-Uphoff, and Steven D. Miller

. J. Atmos. Oceanic Technol. , 33 , 1073 – 1087 , https://doi.org/10.1175/JTECH-D-15-0245.1 . 10.1175/JTECH-D-15-0245.1 Fuchs , B. R. , S. A. Rutledge , B. Dolan , L. D. Carey , and C. Schultz , 2018 : Microphysical and kinematic processes associated with anomalous charge structures in isolated convection . J. Geophys. Res. Atmos. , 123 , 6505 – 6528 , https://doi.org/10.1029/2017JD027540 . 10.1029/2017JD027540 Geer , A. , and Coauthors , 2018 : All-sky satellite data

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Andrew E. Mercer, Alexandria D. Grimes, and Kimberly M. Wood

numerous processes that contribute to TC intensification. Many of these processes are inherently thermodynamic (such as latent heat flux from high sea surface temperatures; Kaplan and DeMaria 2003 ) and not well represented by the dynamic weather models used in operational forecasts ( Kotroni and Lagouvardos 2004 ; Klemp 2006 ; Mercer et al. 2013 ). Kinematic factors relevant to TC intensity change are frequently noisy (e.g., 200-hPa divergence; Leroux 2016 ) or require sufficient vertical

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