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Ya Yang, Xiang Li, Jing Wang, and Dongliang Yuan

the NESC have not been adequately explored so far. The seasonal variability of the Pacific equatorial subsurface currents has been studied by Lukas and Firing (1985) , Kessler and McCreary (1993) , and Marin et al. (2010) , showing that the annual reversal of the Equatorial Intermediate Current is controlled by vertical propagation of baroclinic Rossby waves. Using Argo parking depth trajectory measurements, Cravatte et al. (2012) showed that the largely one cycle per year variations of the

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Dongliang Yuan, Xiang Li, Zheng Wang, Yao Li, Jing Wang, Ya Yang, Xiaoyue Hu, Shuwen Tan, Hui Zhou, Adhitya Kusuma Wardana, Dewi Surinati, Adi Purwandana, Mochamad Furqon Azis Ismail, Praditya Avianto, Dirham Dirhamsyah, Zainal Arifin, and Jin-Song von Storch

( https://verc.enes.org/storm ). Eighty vertical layers from the sea surface to 6038.5 m are used in the vertical. The model was spun up for 25 years using the German Ocean Model Intercomparison Project (OMIP) forcing derived from the 15-yr ERA data and then forced by the 6-hourly NCEP–NCAR reanalysis data from 1948 to present. 3. Observed currents in the Maluku Channel The current data at the center of the Maluku Channel (M00) show a prominent seasonal cycle in the upper ocean above approximately the

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