Interannual Variations of the β Drift of Tropical Cyclones over the Western North Pacific

Author:

Lu Jun1,Wu Liguang234,Zhou Shunwu1,Zhao Haikun1

Affiliation:

1. a Key Laboratory of Meteorological Disaster, Nanjing University of Information Science and Technology, Nanjing, China

2. b Department of Atmospheric and Oceanic Sciences, Fudan University, Shanghai, China

3. c Institute of Atmospheric Sciences, Fudan University, Shanghai, China

4. d Innovation Center of Ocean and Atmosphere System, Zhuhai Fudan Innovation Research Institute, Zhuhai, China

Abstract

Abstract Tropical cyclone (TC) movement consists essentially of the large-scale environmental steering and the β drift, and the latter is also affected by large-scale environmental flows. However, few previous studies have been conducted to examine the interannual variations of the β drift of TCs in the western North Pacific (WNP) basin and the corresponding relationship with the large-scale environmental flow. Using the observed TC tracks and reanalysis dataset during 1965–2019, it is found that the β drift plays a more important role in the TC motion than environmental steering at the interannual time scale. The westward (northward) component of the β drift in the environment with anticyclonic relative vorticity is slower (faster) than that with cyclonic relative vorticity, while an equatorward (poleward) relative vorticity gradient decreases (increases) the westward component of the β drift, in agreement with previous numerical simulations. It is also found that the southwestward migration of the WNP subtropical high can decrease (increase) the westward (northward) component of the β drift. This study suggests that environmental influence on the β drift should be considered when understanding interannual variations of TC movement and tracks, which are important to TC landfall, emergency management, and hazard mitigation. Significance Statement The β drift is an important component of TC movement and is affected by large-scale environmental flows. However, few previous studies have been conducted to examine the interannual variations of the β drift of TCs in the western North Pacific basin and the corresponding relationship with the large-scale environmental flow. This study finds that the β drift plays a more important role in the TC motion than environmental steering at the interannual time scale, and the interannual variations of the β drift are also controlled by large-scale environmental flows. It is suggested that environmental influence on the β drift should be considered when understanding interannual variations of TC movement and tracks, which are important to TC landfall, emergency management, and hazard mitigation.

Funder

National Natural Science Foundation of China

Publisher

American Meteorological Society

Subject

Atmospheric Science

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