Volume 41 Issue 2
Feb.  2022
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Xia Liu, Qiang Wang, Mu Mu. Identifying the sensitive areas in targeted observation for predicting the Kuroshio large meander path in a regional ocean model[J]. Acta Oceanologica Sinica, 2022, 41(2): 3-14. doi: doi:10.1007/s13131-021-1838-7
Citation: Xia Liu, Qiang Wang, Mu Mu. Identifying the sensitive areas in targeted observation for predicting the Kuroshio large meander path in a regional ocean model[J]. Acta Oceanologica Sinica, 2022, 41(2): 3-14. doi: doi:10.1007/s13131-021-1838-7

Identifying the sensitive areas in targeted observation for predicting the Kuroshio large meander path in a regional ocean model

doi: doi:10.1007/s13131-021-1838-7
Funds:  The National Natural Science Foundation of China under contract Nos 41906003 and 41906022; the Strategic Priority Research Program of Chinese Academy of Sciences under contract No. XDA20060502; the Fundamental Research Funds for the Central Universities under contract No. B200201011; the Basic Research Projects of Key Scientific Research Projects Plan in Henan Higher Education Institutions under contract No. 20zx003.
More Information
  • Corresponding author: E-mail: wangq@hhu.edu.cn
  • Received Date: 2021-01-15
  • Accepted Date: 2021-03-30
  • Available Online: 2021-11-25
  • Publish Date: 2022-02-01
  • With the Regional Ocean Modeling System (ROMS), this paper investigates the sensitive areas in targeted observation for predicting the Kuroshio large meander (LM) path using the conditional nonlinear optimal perturbation approach. To identify the sensitive areas, the optimal initial errors (OIEs) featuring the largest nonlinear evolution in the LM prediction are first calculated; the resulting OIEs are localized mainly in the upper 2 500 m over the LM upstream region, and their spatial structure has certain similarities with that of the optimal triggering perturbation. Based on this spatial structure, the sensitive areas are successfully identified, located southeast of Kyushu in the region (29°–32°N, 131°–134°E). A series of sensitivity experiments indicate that both the positions and the spatial structure of initial errors have important effects on the LM prediction, verifying the validity of the sensitive areas. Then, the effect of targeted observation in the sensitive areas is evaluated through observing system simulation experiments. When targeted observation is implemented in the identified sensitive areas, the prediction errors are effectively reduced, and the prediction skill of the LM event is improved significantly. This provides scientific guidance for ocean observations related to enhancing the prediction skill of the LM event.
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  • [1]
    Farrara J D, Chao Yi, Li Zhijin, et al. 2013. A data-assimilative ocean forecasting system for the Prince William sound and an evaluation of its performance during sound Predictions 2009. Continental Shelf Research, 63(S1): S193–S208. doi: 10.1016/j.csr.2012.11.008
    [2]
    Fujii Y, Tsujino H, Usui N, et al. 2008. Application of singular vector analysis to the Kuroshio large meander. Journal of Geophysical Research: Oceans, 113(C7): C07026. doi: 10.1029/2007JC004476
    [3]
    Halliwell Jr R G, Srinivasan A, Kourafalou V, et al. 2014. Rigorous evaluation of a fraternal twin ocean OSSE system for the open Gulf of Mexico. Journal of Atmospheric and Oceanic Technology, 31(1): 105–130. doi: 10.1175/JTECH-D-13-00011.1
    [4]
    Hayasaki M, Kawamura R, Mori M, et al. 2013. Response of extratropical cyclone activity to the Kuroshio large meander in northern winter. Geophysical Research Letters, 40(11): 2851–2855. doi: 10.1002/grl.50546
    [5]
    Ishikawa Y, Awaji T, Komori N, et al. 2004. Application of sensitivity analysis using an adjoint model for short-range forecasts of the Kuroshio path south of Japan. Journal of Oceanography, 60(2): 293–301. doi: 10.1023/b:joce.0000038335.50080.ff
    [6]
    Kawabe M. 1995. Variations of current path, velocity, and volume transport of the Kuroshio in relation with the large meander. Journal of Physical Oceanography, 25(12): 3103–3117. doi: 10.1175/1520-0485(1995)025<3103:VOCPVA>2.0.CO;2
    [7]
    Langland R H. 2005. Issues in targeted observing. Quarterly Journal of the Royal Meteorological Society, 131(613): 3409–3425. doi: 10.1256/qj.05.130
    [8]
    Li Yineng, Peng Shiqiu, Liu Duanling. 2014. Adaptive observation in the South China Sea using CNOP approach based on a 3-D ocean circulation model and its adjoint model. Journal of Geophysical Research: Oceans, 119(12): 8973–8986. doi: 10.1002/2014JC010220
    [9]
    Liu Xia, Mu Mu, Wang Qiang. 2018a. The nonlinear optimal triggering perturbation of the Kuroshio large meander and its evolution in a regional ocean model. Journal of Physical Oceanography, 48(8): 1771–1786. doi: 10.1175/JPO-D-17-0246.1
    [10]
    Liu Xia, Wang Qiang, Mu Mu. 2018b. Optimal initial error growth in the prediction of the Kuroshio large meander based on a high-resolution regional ocean model. Advances in Atmospheric Sciences, 35(11): 1362–1371. doi: 10.1007/s00376-018-8003-z
    [11]
    Ma Xiaohui, Jing Zhao, Chang Ping, et al. 2016. Western boundary currents regulated by interaction between ocean eddies and the atmosphere. Nature, 535(7613): 533–537. doi: 10.1038/nature18640
    [12]
    Miyazawa Y, Kagimoto T, Guo Xinyu, et al. 2008. The Kuroshio large meander formation in 2004 analyzed by an eddy-resolving ocean forecast system. Journal of Geophysical Research: Oceans, 113(C10): C10015. doi: 10.1029/2007JC004226
    [13]
    Miyazawa Y, Yamane S, Guo Xinyu, et al. 2005. Ensemble forecast of the Kuroshio meandering. Journal of Geophysical Research: Oceans, 110(C10): C10026. doi: 10.1029/2004JC002426
    [14]
    Mu Mu. 2013. Methods, current status, and prospect of targeted observation. Science China: Earth Sciences, 56(12): 1997–2005. doi: 10.1007/s11430-013-4727-x
    [15]
    Mu Mu, Duan Wansuo, Wang B. 2003. Conditional nonlinear optimal perturbation and its applications. Nonlinear Processes in Geophysics, 10(6): 493–501. doi: 10.5194/npg-10-493-2003
    [16]
    Mu Mu, Zhou Feifan, Wang Hongli. 2009. A method for identifying the sensitive areas in targeted observations for tropical cyclone prediction: conditional nonlinear optimal perturbation. Monthly Weather Review, 137(5): 1623–1639. doi: 10.1175/2008MWR2640.1
    [17]
    Nakamura H, Nishina A, Minobe S. 2012. Response of storm tracks to bimodal Kuroshio path states south of Japan. Journal of Climate, 25(21): 7772–7779. doi: 10.1175/JCLI-D-12-00326.1
    [18]
    Qin Xiaohao, Mu Mu. 2011. A study on the reduction of forecast error variance by three adaptive observation approaches for tropical cyclone prediction. Monthly Weather Review, 139(7): 2218–2232. doi: 10.1175/2010MWR3327.1
    [19]
    Shao Quanqin, Ma Weiwei, Chen Zhuoqi, et al. 2005. Relationship between Kuroshio meander pattern and Ommastrephes bartrami CPUE in northwest Pacific Ocean. Oceanologia et Limnologia Sinica, 36(2): 111–122
    [20]
    Shchepetkin A F, McWilliams J C. 2003. A method for computing horizontal pressure-gradient force in an oceanic model with a nonaligned vertical coordinate. Journal of Geophysical Research: Oceans, 108(C3): 3090. doi: 10.1029/2001JC001047
    [21]
    Shchepetkin A F, McWilliams J C. 2005. The regional oceanic modeling system (ROMS): a split-explicit, free-surface, topography-following-coordinate oceanic model. Ocean Modelling, 9(4): 347–404. doi: 10.1016/j.ocemod.2004.08.002
    [22]
    Song Yuhe, Haidvogel D. 1994. A semi-implicit ocean circulation model using a generalized topography-following coordinate system. Journal of Computational Physics, 115(1): 228–244. doi: 10.1006/jcph.1994.1189
    [23]
    Taft B A. 1972. Characteristics of the flow of the Kuroshio south of Japan. In: Stommel H, Yoshida K, eds. Kuroshio-Its Physical Aspects. Tokyo, Japan: University of Tokyo Press, 165–216
    [24]
    Tang Youmin, Kleeman R, Moore A M. 2004. SST assimilation experiments in a tropical Pacific Ocean model. Journal of Physical Oceanography, 34(3): 623–642. doi: 10.1175/3518.1
    [25]
    Tsujino H, Usui N, Nakano H. 2006. Dynamics of Kuroshio path variations in a high-resolution general circulation model. Journal of Geophysical Research: Oceans, 111(C11): C11001. doi: 10.1029/2005JC003118
    [26]
    Usui N, Tsujino H, Nakano H. 2008. Formation process of the Kuroshio large meander in 2004. Journal of Geophysical Research: Oceans, 113(C8): C08047. doi: 10.1029/2007JC004675
    [27]
    Wang Qiang, Ma Libin, Xu Qiangqiang. 2013a. Optimal precursor of the transition from Kuroshio large meander to straight path. Chinese Journal of Oceanology and Limnology, 31(5): 1153–1161. doi: 10.1007/s00343-013-2301-1
    [28]
    Wang Qiang, Mu Mu, Dijkstra H A. 2012. Application of the conditional nonlinear optimal perturbation method to the predictability study of the Kuroshio large meander. Advances in Atmospheric Sciences, 29(1): 118–134. doi: 10.1007/s00376-011-0199-0
    [29]
    Wang Qiang, Mu Mu, Dijkstra H A. 2013b. The similarity between optimal precursor and optimally growing initial error in prediction of Kuroshio large meander and its application to targeted observation. Journal of Geophysical Research: Oceans, 118(2): 869–884. doi: 10.1002/jgrc.20084
    [30]
    Wang Qiang, Mu Mu, Dijkstra H A. 2013c. Effects of nonlinear physical processes on optimal error growth in predictability experiments of the Kuroshio Large Meander. Journal of Geophysical Research: Oceans, 118(12): 6425–6436. doi: 10.1002/2013JC009276
    [31]
    Xia Ruibin, Liu Qinyu, Xu Lixiao. 2013. Formation mechanisms of the three Kuroshio large meanders. Periodical of Ocean University of China, 43(5): 1–7
    [32]
    Xu Haiming, Tokinaga H, Xie Shangping. 2010. Atmospheric effects of the Kuroshio large meander during 2004–05. Journal of Climate, 23(17): 4704–4715. doi: 10.1175/2010JCLI3267.1
    [33]
    Yang Yang, Liang Xiangsan. 2019. New perspectives on the generation and maintenance of the Kuroshio large meander. Journal of Physical Oceanography, 49(8): 2095–2113. doi: 10.1175/JPO-D-18-0276.1
    [34]
    Zhang Kun, Mu Mu, Wang Qiang. 2017. Identifying the sensitive area in adaptive observation for predicting the upstream Kuroshio transport variation in a 3-D ocean model. Science China: Earth Sciences, 60(5): 866–875. doi: 10.1007/s11430-016-9020-8
    [35]
    Zou Guangan, Wang Qiang, Mu Mu. 2016. Identifying sensitive areas of adaptive observations for prediction of the Kuroshio large meander using a shallow-water model. Chinese Journal of Oceanology and Limnology, 34(5): 1122–1133. doi: 10.1007/s00343-016-4264-5
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