A statistical comparison of the potential intensity index for tropical cyclones over the Western North Pacific
Abstract Potential intensity (PI), an upper thermodynamic limit of tropical cyclone (TC) intensity, is a useful index in TC statistical forecasting. This study evaluated the relationship between the current intensity of TCs and four PI indexes calculated with different sea surface indicators over th...
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Online Access: | https://doi.org/10.1002/asl.945 |
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doaj-9e80cc766ebf4d81bd85872a74dd84f32020-11-24T21:21:05ZengWileyAtmospheric Science Letters1530-261X2020-01-01211n/an/a10.1002/asl.945A statistical comparison of the potential intensity index for tropical cyclones over the Western North PacificLu Yang0Xiao Gang Huang1Jian Fang Fei2Xiao Ping Cheng3Ju Li Ding4Wen Li Shi5College of Meteorology and Oceanography, National University of Defense Technology Nanjing Jiangsu ChinaCollege of Meteorology and Oceanography, National University of Defense Technology Nanjing Jiangsu ChinaCollege of Meteorology and Oceanography, National University of Defense Technology Nanjing Jiangsu ChinaCollege of Meteorology and Oceanography, National University of Defense Technology Nanjing Jiangsu ChinaCollege of Meteorology and Oceanography, National University of Defense Technology Nanjing Jiangsu ChinaArmy Academy of Artillery and Air Defense (Nanjing Campus) Nanjing Jiangsu ChinaAbstract Potential intensity (PI), an upper thermodynamic limit of tropical cyclone (TC) intensity, is a useful index in TC statistical forecasting. This study evaluated the relationship between the current intensity of TCs and four PI indexes calculated with different sea surface indicators over the Western North Pacific (WNP) from 2009 to 2016. To mirror the degree of sea cooling caused by TCs, three sea surface temperature (SST) indicators (pre‐SST, 80 m depth mean sea temperature, and dynamic mixed mean sea temperature) were compared with real‐time SST obtained from HYbrid Coordinate Ocean Model (HYCOM) data. The results showed that four versions of PI all overestimated the current intensity of developing TCs. In contrast, when a TC at its strongest or in its weakening stages in a favorable atmospheric environment, pre‐sea conditions were strongly correlated with TC intensity. For strong TCs, the ocean‐coupled PI index was best able to describe TC intensity.https://doi.org/10.1002/asl.945potential intensitysea coolingtropical cyclone |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Lu Yang Xiao Gang Huang Jian Fang Fei Xiao Ping Cheng Ju Li Ding Wen Li Shi |
spellingShingle |
Lu Yang Xiao Gang Huang Jian Fang Fei Xiao Ping Cheng Ju Li Ding Wen Li Shi A statistical comparison of the potential intensity index for tropical cyclones over the Western North Pacific Atmospheric Science Letters potential intensity sea cooling tropical cyclone |
author_facet |
Lu Yang Xiao Gang Huang Jian Fang Fei Xiao Ping Cheng Ju Li Ding Wen Li Shi |
author_sort |
Lu Yang |
title |
A statistical comparison of the potential intensity index for tropical cyclones over the Western North Pacific |
title_short |
A statistical comparison of the potential intensity index for tropical cyclones over the Western North Pacific |
title_full |
A statistical comparison of the potential intensity index for tropical cyclones over the Western North Pacific |
title_fullStr |
A statistical comparison of the potential intensity index for tropical cyclones over the Western North Pacific |
title_full_unstemmed |
A statistical comparison of the potential intensity index for tropical cyclones over the Western North Pacific |
title_sort |
statistical comparison of the potential intensity index for tropical cyclones over the western north pacific |
publisher |
Wiley |
series |
Atmospheric Science Letters |
issn |
1530-261X |
publishDate |
2020-01-01 |
description |
Abstract Potential intensity (PI), an upper thermodynamic limit of tropical cyclone (TC) intensity, is a useful index in TC statistical forecasting. This study evaluated the relationship between the current intensity of TCs and four PI indexes calculated with different sea surface indicators over the Western North Pacific (WNP) from 2009 to 2016. To mirror the degree of sea cooling caused by TCs, three sea surface temperature (SST) indicators (pre‐SST, 80 m depth mean sea temperature, and dynamic mixed mean sea temperature) were compared with real‐time SST obtained from HYbrid Coordinate Ocean Model (HYCOM) data. The results showed that four versions of PI all overestimated the current intensity of developing TCs. In contrast, when a TC at its strongest or in its weakening stages in a favorable atmospheric environment, pre‐sea conditions were strongly correlated with TC intensity. For strong TCs, the ocean‐coupled PI index was best able to describe TC intensity. |
topic |
potential intensity sea cooling tropical cyclone |
url |
https://doi.org/10.1002/asl.945 |
work_keys_str_mv |
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