Observation system simulation experiments using an ensemble-based method in the northeastern South China Sea

Wu GENG; Feng CHENG; Qiang XIE; Xiaoli ZOU; Weihong HE; Zhaozheng WANG; Yeqiang SHU; Gengxin CHEN; Danian LIU; Dong YE; Ruiwen WANG; Chuanyu LIU

doi:10.1007/s00343-019-9119-4

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Observation system simulation experiments using an ensemble-based method in the northeastern South China Sea

Physics | Updated：2023-04-27

- Observation system simulation experiments using an ensemble-based method in the northeastern South China Sea
- Observation system simulation experiments using an ensemble-based method in the northeastern South China Sea
- 海洋湖沼学报（英文） 2020年38卷第6期页码：1729-1745
- Affiliations：
  
  1.State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences(SCSIO), Guangzhou 510301, China
  2.China General Nuclear Power, Yangjiang Nuclear Power Co., Ltd., Yangjiang 529941, China
  3.Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
  4.Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya 572000, China
  5.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
  6.Public Weather Service Center of China Meteorological Administration, Beijing 100081, China
  7.National Meteorological Center of China Meteorological Administration, Beijing 100081, China
  8.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences(IOCAS), Qingdao 266071, China
  9.Marine Dynamic Process and Climate Function Laboratory, Pilot National Laboratory for Marine Science and Technology(Qingdao)(QNLM), Qingdao 266237, China
- Author bio：
  
  XIE Qiang, gordonxie@idsse.ac.cn
- Funds：
  
  the National Key R&D Program of China(2016YFC1401703);the National Key R&D Program of China(2016YFC1401702);the National Key Research & Development Plan of China(2018YFC0309803);the National Natural Science Foundation of China(41506002);the National Natural Science Foundation of China(41676010);the National Natural Science Foundation of China(41476011);the National Natural Science Foundation of China(41676015);the National Natural Science Foundation of China (NSFC)(41606026);the Institution of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences(ISEE2019ZR0);the Guangzhou Science and Technology Foundation(201804010133);© Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2020
- DOI：10.1007/s00343-019-9119-4
  中图分类号：
- 收稿：2019-05-07，
  
  录用：2019-6-25，
  
  网络首发：2020-10-30，
  
  纸质出版：2020-11
- Accepted：
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Observation system simulation experiments using an ensemble-based method in the northeastern South China Sea[J]. 海洋湖沼学报（英文）, 2020,38(6):1729-1745.

Wu GENG, Feng CHENG, Qiang XIE, et al. Observation system simulation experiments using an ensemble-based method in the northeastern South China Sea[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1729-1745.
Observation system simulation experiments using an ensemble-based method in the northeastern South China Sea[J]. 海洋湖沼学报（英文）, 2020,38(6):1729-1745. DOI： 10.1007/s00343-019-9119-4.

Wu GENG, Feng CHENG, Qiang XIE, et al. Observation system simulation experiments using an ensemble-based method in the northeastern South China Sea[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1729-1745. DOI： 10.1007/s00343-019-9119-4.

摘要

Abstract

An ensemble-based method for the observation system simulation experiment (OSSE) is employed to design optimal observation stations and assess the present observation stations in the northeastern South China Sea (SCS). We employed the 20-year (1992-2012) sea surface height (SSH) data to design an array to monitor the intraseasonal to interannual variability. The results show that the most key region was found located at the northwest of Luzon Island (LI) where the energetic Luzon cyclonic gyre (LCG) occurs; other key regions include the edge of the LCG

the northwest of the Luzon Strait (LS)

and the southwest of Taiwan

China. By contrast

we found that the present observation stations might oversample at the northwest of the LS and undersample at the northwest of LI. In addition

the optimal stations perform better in a larger area than the present stations. In vertical direction

the key layer is located within the upper 200-m depth

of which the surface and subsurface layers are most valuable to the observing system.

关键词

Keywords

references

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