Atmospheric and oceanic responses to Super Typhoon Mangkhut in the South China Sea: a coupled CROCO-WRF simulation

Mingyu LI; Yijun HE; Guoqiang LIU

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Atmospheric and oceanic responses to Super Typhoon Mangkhut in the South China Sea: a coupled CROCO-WRF simulation

Physics | Updated：2024-10-14

- Atmospheric and oceanic responses to Super Typhoon Mangkhut in the South China Sea: a coupled CROCO-WRF simulation
- Atmospheric and oceanic responses to Super Typhoon Mangkhut in the South China Sea: a coupled CROCO-WRF simulation
- 海洋湖沼学报(英文) 2023年41卷第4期页码：1369-1388
- Affiliations：
  
  1.School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China
  2.Marine Science and Engineering Guangdong Laboratory, Zhuhai 519000, China
  3.Department of Engineering Mathematics and Internetworking, Dalhousie University, Halifax B3H 4R2, Canada
  4.Bedford Institute of Oceanography, Fisheries and Oceans Canada, Dartmouth B2Y 4A2, Canada
- Author bio：
  
  yjhe@nuist.edu.cn
- Funds：
  
  the National Natural Science Foundation of China(41620104003);the Postgraduate Research and Practice Innovation Program of Jiangsu Province (Nos. SJKY19_0951, KYCX21_0959)
- DOI：
  中图分类号：
- 收稿：2021-10-10，
  
  录用：2022-03-31，
  
  网络首发：2022-05-07，
  
  纸质出版：2023-07-01
- Accepted：
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Atmospheric and oceanic responses to Super Typhoon Mangkhut in the South China Sea: a coupled CROCO-WRF simulation[J]. 海洋湖沼学报(英文), 2023,41(4):1369-1388.

LI Mingyu,HE Yijun,LIU Guoqiang.Atmospheric and oceanic responses to Super Typhoon Mangkhut in the South China Sea: a coupled CROCO-WRF simulation[J].Journal of Oceanology and Limnology,2023,41(04):1369-1388.
Atmospheric and oceanic responses to Super Typhoon Mangkhut in the South China Sea: a coupled CROCO-WRF simulation[J]. 海洋湖沼学报(英文), 2023,41(4):1369-1388. DOI：

LI Mingyu,HE Yijun,LIU Guoqiang.Atmospheric and oceanic responses to Super Typhoon Mangkhut in the South China Sea: a coupled CROCO-WRF simulation[J].Journal of Oceanology and Limnology,2023,41(04):1369-1388. DOI：

摘要

Abstract

The South China Sea (SCS) is the largest marginal sea in the Northwest Pacific Ocean

and it encounters frequent typhoons. The atmosphere and ocean will create significant thermal and dynamic responses during the intense disturbance caused by typhoons. However

these responses have not been thoroughly investigated owing to the complicated marine environment. According to the satellite data

the SCS Basin was observed to have a strong sea surface temperature (SST) response to Typhoon Mangkhut

resulting in widespread SST cooling. A coupled model was used to investigate the atmospheric and oceanic responses to Typhoon Mangkhut. Best-track data

satellite SST

and ARGO measurements show that the coupled WRF-CROCO simulation displays better track

intensity

SST

temperature

and salinity profiles than those of the WRF-only simulation. Results show that the typhoon induced rightward intensifications in wind speed

ocean current

and SST. The following are some remarkable atmosphere and ocean responses: (1) the SST below the inner-core region is cooled by 1 °‍‍C

resulting in a 37%‍‍‍–44% decrease in wet enthalpy

and the central pressure is increased by ~9 hPa. Therefore

the changes in SST below the inner-core region of the SCS Basin have a significant impact on air-sea fluxes under high-wind conditions; (2) the ocean boundary layer analysis shows that near-inertial oscillations on the right side of the typhoon track and a strong inertial current up to ~2.28 m/s in the upper ocean were observed

which resonated with the local wind and flow field on the right side and induced strong SST cooling; (3) a decrease in SST decreased the moist static energy of the typhoon boundary layer

thereby weakening the typhoon’s intensity. The difference in equivalent potential temperature and sea surface pressure have a good correlation

indicating that the influence of moist static energy on typhoon intensity cannot be overlooked.

关键词

Keywords

references

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