“…Studies on TC intensity change and rapid intensification (RI) can be classified into three groups such as large-scale atmospheric, oceanic, and TC inner-core processes (Gao et al 2016), which include vertical wind shear, upper-level tropospheric divergence, relative humidity, sea surface temperature, ocean heat content, eyewall replacement, and so on. Characteristics and mechanisms associated with RI have been explored mostly from an operational perspective (Wang and Zhou 2008, Rappaport et al 2012, Elsberry 2014, Emanuel 2017, Wang et al 2017. However, real-time forecasting of TC RI remains a big challenge as the myriad physical mechanisms and their environmental connections need greater clarification (Elsberry et al 2007, Kaplan et al 2010, Lin et al 2013, Rogers et al 2013.…”