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Tropical Cyclone Intensification Simulated in the Ooyama-Type Three-Layer Model with a Multilevel Boundary Layer

Source: Journal of the Atmospheric Sciences:;2021:;volume( 078 ):;issue: 011:;page 3799

Author(s): Fei, Rong;Wang, Yuqing

Publisher: American Meteorological Society

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How Does Horizontal Diffusion Influence the Intensification and Maximum Intensity of Numerically Simulated Tropical Cyclones?

Source: Journal of the Atmospheric Sciences:;2023:;volume( 080 ):;issue: 003:;page 705

Author(s): Fei, Rong; Wang, Yuqing

Publisher: American Meteorological Society

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Contribution of Vertical Advection to Supergradient Wind in Tropical Cyclone Boundary Layer: A Numerical Study

Source: Journal of the Atmospheric Sciences:;2021:;volume( 078 ):;issue: 004:;page 1057

Author(s): Fei, Rong;Wang, Yuqing;Li, Yuanlong

Publisher: American Meteorological Society

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How Does Horizontal Diffusion Influence the Intensification and Maximum Intensity of Numerically Simulated Tropical Cyclones?

Source: Journal of the Atmospheric Sciences:;2023:;volume( 080 ):;issue: 003

Author(s): Fei, Rong; Wang, Yuqing

Publisher: American Meteorological Society

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Dependence of Superintensity of Tropical Cyclones on SST in Axisymmetric Numerical Simulations

Source: Monthly Weather Review:;2020:;volume( 148 ):;issue: 012:;page 4767

Author(s): Li, Yuanlong;Wang, Yuqing;Lin, Yanluan;Fei, Rong

Publisher: American Meteorological Society

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Factors Affecting the Weakening Rate of Tropical Cyclones over the Western North Pacific

Source: Monthly Weather Review:;2020:;volume( 148 ):;issue: 009:;page 3693

Author(s): Fei, Rong;Xu, Jing;Wang, Yuqing;Yang, Chi

Publisher: American Meteorological Society

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Tropical Cyclone Intensification Simulated in the Ooyama-Type Three-Layer Model with a Multilevel Boundary Layer

How Does Horizontal Diffusion Influence the Intensification and Maximum Intensity of Numerically Simulated Tropical Cyclones?

Contribution of Vertical Advection to Supergradient Wind in Tropical Cyclone Boundary Layer: A Numerical Study

How Does Horizontal Diffusion Influence the Intensification and Maximum Intensity of Numerically Simulated Tropical Cyclones?

Dependence of Superintensity of Tropical Cyclones on SST in Axisymmetric Numerical Simulations

Factors Affecting the Weakening Rate of Tropical Cyclones over the Western North Pacific

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Tropical Cyclone Intensification Simulated in the Ooyama-Type Three-Layer Model with a Multilevel Boundary Layer

How Does Horizontal Diffusion Influence the Intensification and Maximum Intensity of Numerically Simulated Tropical Cyclones?

Contribution of Vertical Advection to Supergradient Wind in Tropical Cyclone Boundary Layer: A Numerical Study

How Does Horizontal Diffusion Influence the Intensification and Maximum Intensity of Numerically Simulated Tropical Cyclones?

Dependence of Superintensity of Tropical Cyclones on SST in Axisymmetric Numerical Simulations

Factors Affecting the Weakening Rate of Tropical Cyclones over the Western North Pacific