Editorial Type:
Article
Article Type:
Research Article

Initial Maintenance of Tropical Cyclone Size in the Western North Pacific

Cheng-Shang Lee Department of Atmospheric Sciences, National Taiwan University, and Typhoon and Flood Research Institute, National Applied Research Laboratories, Taipei, Taiwan

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Kevin K. W. Cheung Climate Futures Research Centre, and Department of Environment and Geography, Macquarie University, Sydney, Australia

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Wei-Ting Fang Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan

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Russell L. Elsberry Department of Meteorology, Naval Postgraduate School, Monterey, California

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Print Publication:
01 Aug 2010
DOI:
https://doi.org/10.1175/2010MWR3023.1
Page(s):
3207–3223
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Abstract

A tropical cyclone (TC) size parameter, which is defined here as the radius of 15 m s−1 near-surface wind speed (R15), is calculated for 145 TCs in the western North Pacific during 2000–05 based on QuikSCAT oceanic winds. For the 73 TCs that intensified to typhoon intensity during their lifetimes, the 33% and 67% respective percentiles of R15 at tropical storm intensity and at typhoon intensity are used to categorize small, medium, and large TCs. Whereas many of the small TCs form from an easterly wave synoptic pattern, the monsoon-related formation patterns are favorable for forming medium to large TCs. Most of these 73 TCs stay in the same size category during intensification, which implies specific physical mechanisms for maintaining TC size in the basin. The 18 persistently large TCs from the tropical storm to the typhoon stage mostly have northwestward or north-northwestward tracks, while the 16 persistently small TCs either move westward–northwestward in lower latitudes or develop at higher latitudes with various track types. For the large TCs, strong low-level southwesterly winds exist in the outer core region south of the TC center throughout the intensification period. The small TCs are more influenced by the subtropical high during intensification. The conclusion is that it is the low-level environment that determines the difference between large and small size storms during the early intensification period in the western North Pacific.

Corresponding author address: Kevin K. W. Cheung, Department of Environment and Geography, Macquarie University, Sydney, NSW 2109, Australia. Email: kcheung@els.mq.edu.au

Abstract

A tropical cyclone (TC) size parameter, which is defined here as the radius of 15 m s−1 near-surface wind speed (R15), is calculated for 145 TCs in the western North Pacific during 2000–05 based on QuikSCAT oceanic winds. For the 73 TCs that intensified to typhoon intensity during their lifetimes, the 33% and 67% respective percentiles of R15 at tropical storm intensity and at typhoon intensity are used to categorize small, medium, and large TCs. Whereas many of the small TCs form from an easterly wave synoptic pattern, the monsoon-related formation patterns are favorable for forming medium to large TCs. Most of these 73 TCs stay in the same size category during intensification, which implies specific physical mechanisms for maintaining TC size in the basin. The 18 persistently large TCs from the tropical storm to the typhoon stage mostly have northwestward or north-northwestward tracks, while the 16 persistently small TCs either move westward–northwestward in lower latitudes or develop at higher latitudes with various track types. For the large TCs, strong low-level southwesterly winds exist in the outer core region south of the TC center throughout the intensification period. The small TCs are more influenced by the subtropical high during intensification. The conclusion is that it is the low-level environment that determines the difference between large and small size storms during the early intensification period in the western North Pacific.

Corresponding author address: Kevin K. W. Cheung, Department of Environment and Geography, Macquarie University, Sydney, NSW 2109, Australia. Email: kcheung@els.mq.edu.au

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