2023

(1) Li, Y., Y. Wang, and Z.-M. Tan, 2023: Is the outflow-layer inertial stability crucial to the energy cycle and development of tropical cyclones?  J. Atmos. Sci., 80, 1605–1620.

(2) Wang, Y., Z.-M. Tan, and Y. Li, 2023: Some refinements to the most recent simple time-dependent theory of tropical cyclone intensification and sensitivity.  J. Atmos. Sci., 80, 321–335.

(3) Duan, Z., Y. Wang, and Y. Li, 2023: Effects of sea spray on the simulated tropical cyclone development: dependence on surface drag coefficient parameterization. J. Geophys. Res. Atmospheres, e2022JD037299.

2022

(1) Li, Y., Z.-M. Tan, and Y. Wang, 2022: Relative timing of the ends of hurricane intensification and contraction of the radius of maximum wind in the North Atlantic and Eastern North Pacific. Geophys. Res. Lett., 49, e2022GL101027.

(2) Li, Y., Y. Wang, and Z.-M. Tan, 2022: Why does the initial wind profile inside radius of maximum wind matter to tropical cyclone development? J. Geophys. Res. Atmospheres, 127, e2022JD037039.

(3) Li, Y., Y. Wang, and Z.-M. Tan, 2022: How frequently does rapid intensification occur after rapid contraction of the radius of maximum wind in tropical cyclone over the North Atlantic and Eastern North Pacific? Mon. Wea. Rea., 150, 1747–1760.

2021

(1) Li, Y., Y. Wang, Y. Lin, and X. Wang, 2021: Why does rapid contraction of the radius of maximum wind precede rapid intensification in tropical cyclones? J. Atmos. Sci., 78. 3441–3453.

(2) Fei, R., Y. Wang, and Y. Li, 2021: Contribution of vertical advection to supergradient wind in tropical cyclone boundary layer: A numerical study. J. Atmos. Sci., 78, 1057–1073.

(3) Wang, Y., Y. Li, J. Xu, Z.-M. Tan, and Y. Lin, 2021: The intensity-dependence of tropical cyclone intensification rate in a simplified energetically based dynamical system model. J. Atmos. Sci., 78, 2033–2045.

(4) Wang, Y., Y. Li, and J. Xu, 2021: A new time-dependent theory of tropical cyclone intensification. J. Atmos. Sci., 78, 3855–3865.

(5) Zhao, D., Y. Lin, Y. Li, and X. Gao, 2021: An extreme heat event induced by Typhoon Lekima (2019) and its contributing factors. J. Geophys. Res. Atmospheres, 126, e2021JD034760.

2020

(1) Li, Y., Y. Wang, and Y. Lin, 2020: How much does the upward advection of the supergradient component of boundary layer wind contribute to tropical cyclone intensification and maximum intensity? J. Atmos. Sci., 77, 2649–2664.

(2) Li, Y., Y. Wang, and Y. Lin, 2020: Reply to “Comment on ‘How much does the upward advection of the supergradient component of boundary layer wind contribute to tropical cyclone intensification and maximum intensity?’” J. Atmos. Sci., 77, 4379–4384.

(3) Li, Y., Y. Wang, Y. Lin, and F. Rong, 2020: Dependence of superintensity of tropical cyclone on SST in axisymmetric numerical simulations. Mon. Wea. Rea., 148, 4767–4781.

(4) Li, Y., Y. Wang, Y. Lin, F. Rong, and J. Gao, 2020: Effects of terrain and landmass near Fujian Province of China on the structure and propagation of a long-lived rainband in Typhoon Longwang (2005): A numerical study. J. Geophys. Res. Atmospheres, 125, e2020JD033393.

2019

(1) Li, Y., J.-I. Yano, and Y. Lin, 2019: Is atmospheric convection organized?: Information entropy analysis. Geophys. Astrophys. Fluid Dyn., 113, 553–573.

(2) Li, Y., Y. Lin, and Y. Wang, 2019: A numerical study on the formation and maintenance of a long‐lived rainband in Typhoon Longwang (2005). J. Geophys. Res. Atmospheres, 124, 10401–10426.

(3) Li, Y., Y. Wang, and Y. Lin, 2019: Revisiting the dynamics of eyewall contraction of tropical cyclones. J. Atmos. Sci., 76, 3229–3245.

2018

(1) Lin, Y., Y. Li, Q. Li, M. Chen, F. Xu, Y. Wang, and B. Huang, 2018: A long lasting vortex Rossby wave induced rainband of Typhoon Longwang (2005). Bull. Amer. Meteor. Soc., 99, 1127–1134.