Wednesday, 9 January 2019
Hall 4 (Phoenix Convention Center - West and North Buildings)
Typhoon Nepartak was a category 5 tropical cyclone of 2016 and had significant societal impacts. It went through a rapid intensification (RI), with an increase of maximum wind speed of 51 m s-1 and a decrease of minimum sea level pressure of 74 hPa in 42 h. The real-time forecast from the Coupled Ocean/Atmosphere Mesoscale Prediction System – Tropical Cyclone (COAMPS-TC), starting from 1200 UTC 3 July, predicted the track and intensity reasonably well for Super Typhoon Nepartak and captured the strom’s RI process . A positive feedback among primary and secondary circulations, surface enthalpy fluxes, and mid-level convective heating is demonstrated to be critical for the RI. The storm structure variations seen from the simulated infrared images during RI bear some resemblance to the satellite images from Hamawari-8, although the forecast inner core is broader compared to the observed, presumably due to the relatively coarse resolution used for the real-time forecasts.
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