Impact of warm mesoscale eddy on tropical cyclone intensity

Jia Sun; Guihua Wang; Xuejun Xiong; Zhenli Hui; Xiaomin Hu; Zheng Ling; Long Yu; Guangbing Yang; Yanliang Guo; Xia Ju; Liang Chen

doi:10.1007/s13131-020-1617-x

Volume 39 Issue 8

Aug. 2020

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Jia Sun, Guihua Wang, Xuejun Xiong, Zhenli Hui, Xiaomin Hu, Zheng Ling, Long Yu, Guangbing Yang, Yanliang Guo, Xia Ju, Liang Chen. Impact of warm mesoscale eddy on tropical cyclone intensity[J]. Acta Oceanologica Sinica, 2020, 39(8): 1-13. doi: 10.1007/s13131-020-1617-x

Citation:

Jia Sun, Guihua Wang, Xuejun Xiong, Zhenli Hui, Xiaomin Hu, Zheng Ling, Long Yu, Guangbing Yang, Yanliang Guo, Xia Ju, Liang Chen. Impact of warm mesoscale eddy on tropical cyclone intensity[J]. Acta Oceanologica Sinica, 2020, 39(8): 1-13. doi: 10.1007/s13131-020-1617-x

Citation:

Jia Sun, Guihua Wang, Xuejun Xiong, Zhenli Hui, Xiaomin Hu, Zheng Ling, Long Yu, Guangbing Yang, Yanliang Guo, Xia Ju, Liang Chen. Impact of warm mesoscale eddy on tropical cyclone intensity[J]. Acta Oceanologica Sinica, 2020, 39(8): 1-13. doi: 10.1007/s13131-020-1617-x

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Impact of warm mesoscale eddy on tropical cyclone intensity

doi: 10.1007/s13131-020-1617-x

Jia Sun^{1, 2},
Guihua Wang^{3
,
,},
Xuejun Xiong^{1, 2},
Zhenli Hui^{1, 2},
Xiaomin Hu^{1, 2},
Zheng Ling⁴,
Long Yu^{1, 2},
Guangbing Yang^{1, 2},
Yanliang Guo^{1, 2},
Xia Ju^{1, 2},
Liang Chen^{1, 2, 5}

1.
First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
2.
Laboratory for Regional Oceanography and Numerical Modeling, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
3.
Institute of Atmospheric Sciences, Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China
4.
Guangdong Key Laboratory of Coastal Ocean Variability and Disaster Prediction, Guangdong Ocean University, Zhanjiang 524088, China
5.
College of Oceanic and Atmospheric Sciences, Ocean University of China, Qingdao 266100, China

Funds: The National Natural Science Foundation of China under contract No. 41706034; the Basic Scientific Fund for National Public Research Institutes of China under contract No. 2020Q05; the Open Fund of the Key Laboratory of Ocean Circulation and Waves, Chinese Academy of Sciences under contract Nos KLOCW1803 and KLOCW1804; the Open Fund of the Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology under contract No. 2019A02; the National Natural Science Foundation of China under contract Nos 91428206 and 41376038; the National Science and Technology Major Project under contract No. 2016ZX05057015; the National Programme on Global Change and Air-Sea Interaction under contract Nos GASI-03-01-01-02 and GASI-IPOVAI-01-05; the NSFC-Shandong Joint Fund for Marine Science Research Centers under contract No. U1606405.

More Information

Corresponding author: E-mail: wghocean@yahoo.com
Received Date: 2019-12-25
Accepted Date: 2020-03-05

Available Online: 2020-12-28

Publish Date: 2020-08-25

Abstract

Abstract

The spatial-temporal patterns of tropical cyclone (TC) intensity changes caused by the warm ocean mesoscale eddy (WOME) distribution are evaluated using two sets of idealized numerical experiments. The results show that the TC was intensified and weakened when a WOME was close to and far away from the TC center, respectively. The area where the WOME enhanced (weakened) TC intensity is called the inner (outer) area in this study. Amplitudes of the enhancement and weakening caused by the WOME in the inner and outer area decreased and increased over time, while the ranges of the inner and outer area diminished and expanded, respectively. The WOME in the inner area strengthened the secondary circulation of the TC, increased heat fluxes, strengthened the symmetry, and weakened the outer spiral rainband, which enhanced TC intensity. The effect was opposite if the WOME was in the outer area, and it weakened the TC intensity. The idealized simulation employed a stationary TC, and thus the results may only be applied to TCs with slow propagation. These findings can improve our understanding of the interactions between TC and the WOME and are helpful for improving TC intensity forecasting by considering the effect of the WOME in the outer areas.
- tropical cyclone intensity,
- warm ocean mesoscale eddy,
- upper ocean,
- spatial-temporal pattern

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References(69)

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