J
Jinkai Li
Researcher at South China Normal University
Publications - 74
Citations - 1550
Jinkai Li is an academic researcher from South China Normal University. The author has contributed to research in topics: Primitive equations & Uniqueness. The author has an hindex of 20, co-authored 68 publications receiving 1106 citations. Previous affiliations of Jinkai Li include The Chinese University of Hong Kong & Weizmann Institute of Science.
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Global Well-Posedness of the Three-Dimensional Primitive Equations with Only Horizontal Viscosity and Diffusion
TL;DR: In this paper, the authors considered the initial boundary value problem of the three-dimensional primitive equations for planetary oceanic and atmospheric dynamics with only horizontal eddy viscosity in the horizontal momentum equations and only horizontal diffusion in the temperature equation.
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Global well-posedness of strong solutions to the 3D primitive equations with horizontal eddy diffusivity
TL;DR: In this paper, the authors considered the initial boundary value problem of the 3D primitive equations for oceanic and atmospheric dynamics with only horizontal diffusion in the temperature equation, and established the global well-posedness of strong solutions with H2 initial data.
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Global Well-Posedness of the 2D Boussinesq Equations with Vertical Dissipation
Jinkai Li,Edriss S. Titi +1 more
TL;DR: In this paper, the authors proved the global well-posedness of the Boussinesq equations with only vertical dissipation, where the initial data are required to be only in the space of the Euclidean distance.
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Blow-up Criteria of Strong Solutions to the Ericksen-Leslie System in ℝ3
TL;DR: In this article, the authors established the local wellposedness and blow-up criteria of strong solutions to the Ericksen-Leslie system in ℝ3 for the well-known Oseen-Frank model.
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Local and Global Well-Posedness of Strong Solutions to the 3D Primitive Equations with Vertical Eddy Diffusivity
TL;DR: In this paper, the authors considered the initial-boundary value problem of the viscous 3D primitive equations for oceanic and atmospheric dynamics with only vertical diffusion in the temperature equation.