李元龙 - 南京大学 - 大气科学学院

个人简介

教育经历 2016–2021 – 清华大学博士生态学（大气科学方向） 2018–2020 – 夏威夷大学 (联合培养) 2012–2016 – 云南大学学士大气科学工作经历 2021-至今 – 南京大学博士后研究项目 2023–2025，国家自然科学基金，青年项目，“台风最大风速半径变化的动力学机理研究”（42205001），主持 2022–2026，国家自然科学基金，重大项目，“台风发生发展理论与精细预报技术研究”，课题二：“台风路径、强度和结构变化动力学与可预报性研究”（42192555），骨干 2022–2022，南京大学校级项目，毓秀青年学者计划，台风加强理论研究（14380185），主持 2021–2023，博士后科学基金，面上资助一等，“台风快速增强和眼墙快速收缩的动力关系”（2021M700066），主持 2021–2023，博士后科学基金，博士后创新人才支持计划，“热带气旋加强的内部动力热力机制研究”(BX2021121)，主持

研究领域

热带气旋动力学、热带对流、中尺度数值模拟

近期论文

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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. 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. 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. 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. 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. 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. 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. 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. 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. Wang, Y., Y. Li, and J. Xu, 2021: A new time-dependent theory of tropical cyclone intensification. J. Atmos. Sci., 78, 3855–3865. 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. 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. 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. 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. 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. Li, Y., J.-I. Yano, and Y. Lin, 2019: Is atmospheric convection organized?: Information entropy analysis. Geophys. Astrophys. Fluid Dyn., 113, 553–573. 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. Li, Y., Y. Wang, and Y. Lin, 2019: Revisiting the dynamics of eyewall contraction of tropical cyclones. J. Atmos. Sci., 76, 3229–3245. 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.