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Benjamin C. Trabing and Michael M. Bell

modes of tropical upward motion . Geophys. Res. Lett. , 46 , 2911 – 2921 , . 10.1029/2018GL081806 Ruppert , J. H. , and M. E. O’Neill , 2019 : Diurnal cloud and circulation changes in simulated tropical cyclones . Geophys. Res. Lett. , 46 , 502 – 511 , . 10.1029/2018GL081302 Ruppert , J. H. , A. A. Wing , X. Tang , and E. L. Duran , 2020 : The critical role of cloud–infrared radiation feedback in

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Kyle Chudler, Weixin Xu, and Steven A. Rutledge

TRMM PR data and groups together near-surface raining pixels that are contiguous in space. Once a feature is outlined, the location of the PF is determined as the centroid of an ellipse surrounding the raining pixels. In addition to the three-dimensional PR radar data, measurements from other TRMM instruments ( Kummerow et al. 1998 ) such as the Lightning Imaging Sensor (LIS), Visible and Infrared Scanner (VIRS), and Microwave Imager (TMI) can then be collocated with the PF. Therefore, information

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