Physical Formation Mechanisms of the Southwest China Vortex
On the basis of the Prandtl boundary layer theory and an improved perturbation method, the process of laminar flow bifurcating into the Southwest China vortex (SWV) in the Hengduan Mountains is studied. The results show that the formation of SWV is mainly determined by the speed of incoming airflow...
Main Authors: | Chun Liu, Yueqing Li, Zimu Liu, Molin Ye |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2022-09-01
|
Series: | Atmosphere |
Subjects: | |
Online Access: | https://www.mdpi.com/2073-4433/13/10/1546 |
Similar Items
-
Physical Mechanism of the Development and Extinction of the China Southwest Vortex
by: Wenlin Zhou, et al.
Published: (2023-02-01) -
An index reflecting mesoscale vortex–vortex interaction and its diagnostic applications for rainstorm area
by: Yongren Chen, et al.
Published: (2019-06-01) -
Helicity characteristics of cyclonic vortexes and their effect on convection in a wide‐ranging extreme rainstorm in China
by: Yongren Chen, et al.
Published: (2023-07-01) -
Wake Formation Flow Physics and Boundary Layer Analysis on the Sides of the Isosceles Triangular Cylinder with Apex Pointing Downstream
by: Namit Agrawal, et al.
Published: (2024-04-01) -
Vortex-induced vibrations of a cylinder with tripping wires
by: Hover, F.S., et al.
Published: (2005)