SST effect on the pre-monsoon intraseasonal oscillation over the South China Sea based on atmospheric-coupled GCM comparison

Yun LIANG; Yan DU; Shang-Ping XIE

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SST effect on the pre-monsoon intraseasonal oscillation over the South China Sea based on atmospheric-coupled GCM comparison

Marine ecological environment and its response to marine dynamic processesin the South China Sea | Updated：2024-10-12

- SST effect on the pre-monsoon intraseasonal oscillation over the South China Sea based on atmospheric-coupled GCM comparison
- Journal of Oceanology and Limnology Vol. 41, Issue 2, Pages: 409-417(2023)
- Affiliations：
  
  1.State Key Laboratory of Tropical Oceanography & Key Laboratory of Science and Technology on Operational Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences & Innovation Academy of South China Sea Ecology and Environmental Engineering, Guangzhou 510301, China
  2.College of Marine Science, University of Chinese Academy of Sciences, Beijing 100049, China
  3.Peking University Chongqing Research Institute of Big Data, Chongqing 401332, China
  4.Southern Marine Science and Engineering Guangdong Laboratory, Guangzhou 510301, China
  5.Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
- Author bio：
  
  duyan@scsio.ac.cn
- Funds：
- DOI：
  CLC：
- Received：20 December 2021，
  
  Published：01 March 2023
- Accepted：
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LIANG Yun,DU Yan,XIE Shang-Ping.SST effect on the pre-monsoon intraseasonal oscillation over the South China Sea based on atmospheric-coupled GCM comparison[J].Journal of Oceanology and Limnology,2023,41(02):409-417.
DOI：

LIANG Yun,DU Yan,XIE Shang-Ping.SST effect on the pre-monsoon intraseasonal oscillation over the South China Sea based on atmospheric-coupled GCM comparison[J].Journal of Oceanology and Limnology,2023,41(02):409-417. DOI：

摘要

Abstract

The role of sea surface temperature (SST) variability in the pre-monsoonal (April to July) intraseasonal oscillation (ISO) over the South China Sea (SCS) is investigated using the Community Earth System Model Version 2 (CESM2). An Atmospheric Model Intercomparison Project (AMIP) simulation forced by daily sea surface temperatures (SSTs) derived from a parallel coupled general circulation model (CGCM) run was compared with observations and the mother coupled simulation. In the coupled model

the SST warming leads the peak convection about 1/4 period as in observations. The paralell uncoupled model fails to simulate this phase relationship

implying the importance of air-sea coupling in reproducing realistic ISO. Due to the near-quadrature phase relationship between SST and precipitation ISOs during the ISO events

it is difficult to distinguish the active/passive role of SST from observations alone. Significant correlation in intraseasonal precipitation between the daily SST-forced AMIP and mother CGCM runs indicates that SST plays a role in driving the atmospheric ISO.

关键词

Keywords

references

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