The effects of the full Coriolis force on the structure and motion of a tropical cyclone part I: Effects due to vertical motion

Xudong Liang; Johnny C.L. Chan; Yihong Duan

The effects of the full Coriolis force on the structure and motion of a tropical cyclone part I: Effects due to vertical motion

Xudong Liang
, Johnny C.L. Chan
, Yihong Duan

Research output: Chapters, Conference Papers, Creative and Literary Works › RGC 32 - Refereed conference paper (with host publication) › peer-review

Abstract

The effects of full coriolis force on simulated structure and motion of tropical cyclone (TC) was investigated. The integration of barotropic model gave a positive geopotential height anomoly to the north. The relative vorticity and divergence anomaly distribution were found to be opposite. The geopotential height and relative vorticity distributions dominates in baroclinic model experiment. The effect of Coriolis force included a complex structure with a wavenumber one distribution of the anaomaly fields, intensified structure in the southeastern section in the outer areas and a southwestward displacement.

Original language	English
Title of host publication	26th Conference on Hurricanes and Tropical Meteorology
Pages	661-662
Publication status	Published - 2004
Event	26th Conference on Hurricanes and Tropical Meteorolgy - Miami, FL., United States Duration: 3 May 2004 → 7 May 2004

Conference

Conference	26th Conference on Hurricanes and Tropical Meteorolgy
Place	United States
City	Miami, FL.
Period	3/05/04 → 7/05/04

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@inproceedings{9bff0e0894ad4e5f882fac262b71f9e6,

title = "The effects of the full Coriolis force on the structure and motion of a tropical cyclone part I: Effects due to vertical motion",

abstract = "The effects of full coriolis force on simulated structure and motion of tropical cyclone (TC) was investigated. The integration of barotropic model gave a positive geopotential height anomoly to the north. The relative vorticity and divergence anomaly distribution were found to be opposite. The geopotential height and relative vorticity distributions dominates in baroclinic model experiment. The effect of Coriolis force included a complex structure with a wavenumber one distribution of the anaomaly fields, intensified structure in the southeastern section in the outer areas and a southwestward displacement.",

author = "Xudong Liang and Chan, \{Johnny C.L.\} and Yihong Duan",

year = "2004",

language = "English",

pages = "661--662",

booktitle = "26th Conference on Hurricanes and Tropical Meteorology",

note = "26th Conference on Hurricanes and Tropical Meteorolgy ; Conference date: 03-05-2004 Through 07-05-2004",

}

The effects of the full Coriolis force on the structure and motion of a tropical cyclone part I: Effects due to vertical motion. / Liang, Xudong; Chan, Johnny C.L.; Duan, Yihong.
26th Conference on Hurricanes and Tropical Meteorology. 2004. p. 661-662.

Research output: Chapters, Conference Papers, Creative and Literary Works › RGC 32 - Refereed conference paper (with host publication) › peer-review

TY - GEN

T1 - The effects of the full Coriolis force on the structure and motion of a tropical cyclone part I

T2 - 26th Conference on Hurricanes and Tropical Meteorolgy

AU - Liang, Xudong

AU - Chan, Johnny C.L.

AU - Duan, Yihong

PY - 2004

Y1 - 2004

N2 - The effects of full coriolis force on simulated structure and motion of tropical cyclone (TC) was investigated. The integration of barotropic model gave a positive geopotential height anomoly to the north. The relative vorticity and divergence anomaly distribution were found to be opposite. The geopotential height and relative vorticity distributions dominates in baroclinic model experiment. The effect of Coriolis force included a complex structure with a wavenumber one distribution of the anaomaly fields, intensified structure in the southeastern section in the outer areas and a southwestward displacement.

AB - The effects of full coriolis force on simulated structure and motion of tropical cyclone (TC) was investigated. The integration of barotropic model gave a positive geopotential height anomoly to the north. The relative vorticity and divergence anomaly distribution were found to be opposite. The geopotential height and relative vorticity distributions dominates in baroclinic model experiment. The effect of Coriolis force included a complex structure with a wavenumber one distribution of the anaomaly fields, intensified structure in the southeastern section in the outer areas and a southwestward displacement.

UR - https://www.scopus.com/pages/publications/3042698852

UR - https://www.scopus.com/record/pubmetrics.uri?eid=2-s2.0-3042698852&origin=recordpage

M3 - RGC 32 - Refereed conference paper (with host publication)

SP - 661

EP - 662

BT - 26th Conference on Hurricanes and Tropical Meteorology

Y2 - 3 May 2004 through 7 May 2004

ER -

The effects of the full Coriolis force on the structure and motion of a tropical cyclone part I: Effects due to vertical motion

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