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David R. Ryglicki, Daniel Hodyss, and Gregory Rainwater

: Improvements in the probabilistic prediction of tropical cyclone rapid intensification with passive microwave observations . Wea. Forecasting , 30 , 1016 – 1038 , https://doi.org/10.1175/WAF-D-14-00109.1 . 10.1175/WAF-D-14-00109.1 Ryglicki , D. R. , and R. E. Hart , 2015 : An investigation of center-finding techniques for tropical cyclones in mesoscale models . J. Appl. Meteor. Climatol. , 54 , 825 – 846 , https://doi.org/10.1175/JAMC-D-14-0106.1 . 10.1175/JAMC-D-14-0106.1 Ryglicki , D. R

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Yi Dai, Sharanya J. Majumdar, and David S. Nolan

is used to describe the outflow. This altitude is mostly consistent with findings from aircraft observations ( Komaromi and Doyle 2017 ). However, such a definition is not sufficient to quantitatively relate the full outflow process with TC intensification. We need a simple and meaningful diagnostic to not only represent the direction and strength of the asymmetric outflow, but also to infer the relation between the outflow, environmental flow, and TC intensity. A central hypothesis of our study

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Jonathan Martinez, Michael M. Bell, Robert F. Rogers, and James D. Doyle

) analyzed in this study and its corresponding time window. Observations collected between 1715 and 1915 UTC 22 October as Patricia was in the midst of its record-breaking rapid intensification phase ( Fig. 1a ) are denoted herein as the RI IOP. Microwave imagery shows deep convection in the eyewall wrapping around a compact center of circulation as Patricia had just achieved category 4 status ( Fig. 2a ). Both the P-3 and WB-57 executed figure-4 patterns with the P-3 flying the 700-hPa flight level

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