Contrasts of bimodal tropical instability waves (TIWs)- induced wind stress perturbations in the Pacific Ocean among observations, ocean models, and coupled climate models

Kai MA; Chuanyu LIU; Junli XU; Fan WANG

doi:10.1007/s00343-023-2326-z

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Contrasts of bimodal tropical instability waves (TIWs)- induced wind stress perturbations in the Pacific Ocean among observations, ocean models, and coupled climate models

Physics | Updated：2024-10-15

- Contrasts of bimodal tropical instability waves (TIWs)- induced wind stress perturbations in the Pacific Ocean among observations, ocean models, and coupled climate models
- Journal of Oceanology and Limnology Vol. 42, Issue 1, Pages: 1-23(2024)
- Affiliations：
  
  1.School of Mathematics and Physics, Research Institute for Mathematics and Interdisciplinary Sciences, Qingdao University of Science and Technology, Qingdao 266100, China
  2.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  3.Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
- Author bio：
  
  chuanyu.liu@qdio.ac.cn
- Funds：
- DOI：10.1007/s00343-023-2326-z
  CLC：
- Received：23 September 2022，
  
  Accepted：07 November 2022，
  
  Online First：20 December 2022，
  
  Published：03 January 2024
- Accepted：
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MA Kai,LIU Chuanyu,XU Junli,et al.Research Paper Contrasts of bimodal tropical instability waves (TIWs)- induced wind stress perturbations in the Pacific Ocean among observations, ocean models, and coupled climate models[J].Journal of Oceanology and Limnology,2024,42(01):1-23.
DOI：

MA Kai,LIU Chuanyu,XU Junli,et al.Research Paper Contrasts of bimodal tropical instability waves (TIWs)- induced wind stress perturbations in the Pacific Ocean among observations, ocean models, and coupled climate models[J].Journal of Oceanology and Limnology,2024,42(01):1-23. DOI： 10.1007/s00343-023-2326-z.

摘要

Abstract

The coupling between wind stress perturbations and sea surface temperature (SST) perturbations induced by tropical instability waves (TIWs) in the Pacific Ocean has been revealed previously and proven crucial to both the atmosphere and ocean. However

an overlooked fact by previous studies is that the loosely defined “TIWs” actually consist of two modes

including the Yanai wave-based TIW on the equator (hereafter eTIW) and the Rossby wave-based TIW off the equator (hereafter vTIW). Hence

the individual feedbacks of the wind stress to the bimodal TIWs remain unexplored. In this study

individual coupling relationships are established for both eTIW and vTIW

including the relationship between the TIW-induced SST perturbations and two components of wind stress perturbations

and the relationship between the TIW-induced wind stress perturbation divergence (curl) and the downwind (crosswind) TIW-induced SST gradients. Results show that

due to different distributions of eTIW and vTIW

the coupling strength induced by the eTIW is stronger on the equator

and that by the vTIW is stronger off the equator. The results of any of eTIW and vTIW are higher than those of the loosely defined TIWs. We further investigated how well the coupling relationships remained in several widely recognized oceanic general circulation models and fully coupled climate models. However

the coupling relationships cannot be well represented in most numerical models. Finally

we confirmed that higher resolution usually corresponds to more accurate simulation. Therefore

the coupling models established in this study are complementary to previous research and can be used to refine the oceanic and coupled climate models.

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references

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