Periodic Cycles of Eyewall Convection Limit the Rapid Intensification of Typhoon Hato (2017)

• Published in: Advances in meteorology 2021, Vol.2021, p.1-18
• Main Authors: Fang, Rong, Chen, Shumin, Zhou, Mingsen, Li, Weibiao, Xiao, Hui, Zhan, Tang, Wu, Yusi, Liu, Haoya, Tu, Chaoyong
• Format: Article
• Language: English
• Subjects: Advection; Amplification; Analysis; Convection; Convection processes; Cycles; Cyclones; Enthalpy; Evolution; Heat; Heat transfer; Heating; Hurricanes; Latent heat; Mathematical models; Meteorological research; Numerical analysis; Numerical simulations; Numerical weather forecasting; Potential temperature; Radar; Radiation; Sensible heat; Simulation; South China Sea; Tropical climate; Tropical cyclone intensities; Tropical cyclones; Typhoons; Vertical advection; Vortices; Weather; Weather forecasting
• ISSN: 1687-9309; 1687-9317
• DOI: 10.1155/2021/5557448

The ability to forecast tropical cyclone (TC) intensity has improved modestly in recent years, partly because of an inadequate understanding of eyewall convection processes. Short-term periodic convection activities (period: 3–5 h) have been identified in a number of TCs, but the effect of these activities on the evolution of TC intensity at the hourly scale is yet to be fully investigated. Using radar observations and a high-resolution numerical simulation based on the Weather Research and Forecasting model, we analyzed the periodic cycles of eyewall convection associated with the intensification of Typhoon Hato (2017). Results indicate the presence of four short-term periodic cycles (period: 3–5 h) in the eyewall convection, which correspond to TC intensification. We further divided each cycle into three stages. The periodic evolution of convection inhibited the rapid intensification of the TC. The highest and lowest intensification rates were associated with the first and third stages according to the virtual potential temperature tendency in the eyewall region, respectively. Heating was dominated by the vertical advection associated with sensible heat and latent heat, which were controlled by the eyewall convection and structure. Of the three stages in each cycle, the vertical transport released the largest amount of latent heat in the first stage; consequently, the highest intensification rate occurred in this stage. In the second stage, heating was reduced because of decreased latent heat and increased cooling of sensible heat associated with vertical advection as the eyewall intensified. Vertical transport was the weakest in the third stage; this resulted in the smallest amount of heating, which limited the rapid intensification of the TC.