Impact of Ocean Warming on Tropical Cyclone Size and Its Destructiveness

Abstract The response of tropical cyclone (TC) destructive potential to global warming is an open issue. A number of previous studies have ignored the effect of TC size change in the context of global warming, which resulted in a significant underestimation of the TC destructive potential. The lack...

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Main Authors: Yuan Sun, Zhong Zhong, Tim Li, Lan Yi, Yijia Hu, Hongchao Wan, Haishan Chen, Qianfeng Liao, Chen Ma, Qihua Li
Format: Article
Language:English
Published: Nature Publishing Group 2017-08-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-017-08533-6
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spelling doaj-52242e6a7c394a47b2a419e5c20bc0a62020-12-08T00:59:10ZengNature Publishing GroupScientific Reports2045-23222017-08-017111010.1038/s41598-017-08533-6Impact of Ocean Warming on Tropical Cyclone Size and Its DestructivenessYuan Sun0Zhong Zhong1Tim Li2Lan Yi3Yijia Hu4Hongchao Wan5Haishan Chen6Qianfeng Liao7Chen Ma8Qihua Li9Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environmental Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and TechnologyCollege of Meteorology and Oceanography, National University of Defense TechnologyKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environmental Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and TechnologyChinese Academy of Meteorological Sciences/Chinese Meteorological SocietyCollege of Meteorology and Oceanography, National University of Defense TechnologyMeteorological Observatory of Hankou StationKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environmental Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and TechnologyCollege of Meteorology and Oceanography, National University of Defense TechnologyKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environmental Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and TechnologyCollege of Meteorology and Oceanography, National University of Defense TechnologyAbstract The response of tropical cyclone (TC) destructive potential to global warming is an open issue. A number of previous studies have ignored the effect of TC size change in the context of global warming, which resulted in a significant underestimation of the TC destructive potential. The lack of reliable and consistent historical data on TC size limits the confident estimation of the linkage between the observed trend in TC size and that in sea surface temperature (SST) under the background of global climate warming. A regional atmospheric model is used in the present study to investigate the response of TC size and TC destructive potential to increases in SST. The results show that a large-scale ocean warming can lead to not only TC intensification but also TC expansion. The TC size increase in response to the ocean warming is possibly attributed to the increase in atmospheric convective instability in the TC outer region below the middle troposphere, which facilitates the local development of grid-scale ascending motion, low-level convergence and the acceleration of tangential winds. The numerical results indicate that TCs will become stronger, larger, and unexpectedly more destructive under global warming.https://doi.org/10.1038/s41598-017-08533-6
collection DOAJ
language English
format Article
sources DOAJ
author Yuan Sun
Zhong Zhong
Tim Li
Lan Yi
Yijia Hu
Hongchao Wan
Haishan Chen
Qianfeng Liao
Chen Ma
Qihua Li
spellingShingle Yuan Sun
Zhong Zhong
Tim Li
Lan Yi
Yijia Hu
Hongchao Wan
Haishan Chen
Qianfeng Liao
Chen Ma
Qihua Li
Impact of Ocean Warming on Tropical Cyclone Size and Its Destructiveness
Scientific Reports
author_facet Yuan Sun
Zhong Zhong
Tim Li
Lan Yi
Yijia Hu
Hongchao Wan
Haishan Chen
Qianfeng Liao
Chen Ma
Qihua Li
author_sort Yuan Sun
title Impact of Ocean Warming on Tropical Cyclone Size and Its Destructiveness
title_short Impact of Ocean Warming on Tropical Cyclone Size and Its Destructiveness
title_full Impact of Ocean Warming on Tropical Cyclone Size and Its Destructiveness
title_fullStr Impact of Ocean Warming on Tropical Cyclone Size and Its Destructiveness
title_full_unstemmed Impact of Ocean Warming on Tropical Cyclone Size and Its Destructiveness
title_sort impact of ocean warming on tropical cyclone size and its destructiveness
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2017-08-01
description Abstract The response of tropical cyclone (TC) destructive potential to global warming is an open issue. A number of previous studies have ignored the effect of TC size change in the context of global warming, which resulted in a significant underestimation of the TC destructive potential. The lack of reliable and consistent historical data on TC size limits the confident estimation of the linkage between the observed trend in TC size and that in sea surface temperature (SST) under the background of global climate warming. A regional atmospheric model is used in the present study to investigate the response of TC size and TC destructive potential to increases in SST. The results show that a large-scale ocean warming can lead to not only TC intensification but also TC expansion. The TC size increase in response to the ocean warming is possibly attributed to the increase in atmospheric convective instability in the TC outer region below the middle troposphere, which facilitates the local development of grid-scale ascending motion, low-level convergence and the acceleration of tangential winds. The numerical results indicate that TCs will become stronger, larger, and unexpectedly more destructive under global warming.
url https://doi.org/10.1038/s41598-017-08533-6
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