Rapid Growth of Tropical Cyclone Outer Size over the Western North Pacific

The concept of rapid growth (RG) of tropical cyclones (TCs) in the north Atlantic basin was recently proposed. RG can represent a dangerous change in TC structure because it can rapidly ramp up the TC destructive potential. However, the nature of RG behaviour remains obscure over the western north P...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Yi Li, Youmin Tang, Shuai Wang, Xiaojing Li
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15020486
id ftmdpi:oai:mdpi.com:/2072-4292/15/2/486/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2072-4292/15/2/486/ 2023-08-20T04:08:18+02:00 Rapid Growth of Tropical Cyclone Outer Size over the Western North Pacific Yi Li Youmin Tang Shuai Wang Xiaojing Li agris 2023-01-13 application/pdf https://doi.org/10.3390/rs15020486 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Remote Sensing https://dx.doi.org/10.3390/rs15020486 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 2; Pages: 486 tropical cyclone western north Pacific rapid growth outer size Text 2023 ftmdpi https://doi.org/10.3390/rs15020486 2023-08-01T08:17:45Z The concept of rapid growth (RG) of tropical cyclones (TCs) in the north Atlantic basin was recently proposed. RG can represent a dangerous change in TC structure because it can rapidly ramp up the TC destructive potential. However, the nature of RG behaviour remains obscure over the western north Pacific (WNP), where nearly one third of global TCs occur. In this study, TC RG in the WNP is investigated using TC best-tracks and reanalysis of data. We first define TC RG in the WNP as an increase of at least 84 km in the radius of a gale-force wind within 24 h, corresponding to the 90th percentile of all over-water changes. Monte Carlo experiments demonstrate the robustness of the threshold. Similar to that occurring in the north Atlantic, RG in the WNP is associated with the highest level of destructive potential. In addition, RG over the WNP occurs closer to the coast than for TCs in the Atlantic and more RG events in the WNP are accompanied by rapid intensification, which may significantly increase their destructive potential in a worst case scenario. Composite analysis shows that certain dynamic processes, such as radial inflow, may play an important role in the occurrence of RG. This study suggests that, apart from rapid intensification, TC RG is another important factor to consider for TC-related risk assessment in the WNP. Text North Atlantic MDPI Open Access Publishing Pacific Remote Sensing 15 2 486
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic tropical cyclone
western north Pacific
rapid growth
outer size
spellingShingle tropical cyclone
western north Pacific
rapid growth
outer size
Yi Li
Youmin Tang
Shuai Wang
Xiaojing Li
Rapid Growth of Tropical Cyclone Outer Size over the Western North Pacific
topic_facet tropical cyclone
western north Pacific
rapid growth
outer size
description The concept of rapid growth (RG) of tropical cyclones (TCs) in the north Atlantic basin was recently proposed. RG can represent a dangerous change in TC structure because it can rapidly ramp up the TC destructive potential. However, the nature of RG behaviour remains obscure over the western north Pacific (WNP), where nearly one third of global TCs occur. In this study, TC RG in the WNP is investigated using TC best-tracks and reanalysis of data. We first define TC RG in the WNP as an increase of at least 84 km in the radius of a gale-force wind within 24 h, corresponding to the 90th percentile of all over-water changes. Monte Carlo experiments demonstrate the robustness of the threshold. Similar to that occurring in the north Atlantic, RG in the WNP is associated with the highest level of destructive potential. In addition, RG over the WNP occurs closer to the coast than for TCs in the Atlantic and more RG events in the WNP are accompanied by rapid intensification, which may significantly increase their destructive potential in a worst case scenario. Composite analysis shows that certain dynamic processes, such as radial inflow, may play an important role in the occurrence of RG. This study suggests that, apart from rapid intensification, TC RG is another important factor to consider for TC-related risk assessment in the WNP.
format Text
author Yi Li
Youmin Tang
Shuai Wang
Xiaojing Li
author_facet Yi Li
Youmin Tang
Shuai Wang
Xiaojing Li
author_sort Yi Li
title Rapid Growth of Tropical Cyclone Outer Size over the Western North Pacific
title_short Rapid Growth of Tropical Cyclone Outer Size over the Western North Pacific
title_full Rapid Growth of Tropical Cyclone Outer Size over the Western North Pacific
title_fullStr Rapid Growth of Tropical Cyclone Outer Size over the Western North Pacific
title_full_unstemmed Rapid Growth of Tropical Cyclone Outer Size over the Western North Pacific
title_sort rapid growth of tropical cyclone outer size over the western north pacific
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15020486
op_coverage agris
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source Remote Sensing; Volume 15; Issue 2; Pages: 486
op_relation Atmospheric Remote Sensing
https://dx.doi.org/10.3390/rs15020486
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15020486
container_title Remote Sensing
container_volume 15
container_issue 2
container_start_page 486
_version_ 1774720484691148800