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Summary Report Lecturer: Chia-Ping Chiang Date: 2009/Jun/25
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Model Description ~ The Whole Domain
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The whole model domain covers entire North Pacific Ocean ranging from 100°E to 80°W and from 30°S to 60°N. A 1/4° horizontal resolution is used east of 150°E, while a finer horizontal resolution of 1/8° is used west of 150°E. The vertical resolution is linear-exponential stretched grid of 26 layers with a thickness of 6 meter in the top layer. Both domains use the same vertical grids. Model bathymetry: Interpolated from unfiltered ETOPO-5 depth data. Supplemented with the Taiwan’s National Center for Ocean Research’s (NCOR) 1- minute high accuracy depth archive in the Asian Seas. The surface wind forcing: Interpolated monthly Hellerman and Rosenstein winds stress. Surface sources of heat and fresh water: The Levitus94 seasonal climatology is used to initialize the model. The eddy viscosity (A h, A v ) and diffusivity (K h, K v ) used in both domains are 20 m 2 /sec. Model Validation ~ The System Settings
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Conservation of Mass Momentum equations (Horizontal) Hydrostatic equation (Vertical) Equation of conservation of salt or energy (potential temperature) Equation of State (EOS): Model Validation ~ The Governing Equations
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Model Description ~ The TAI Domain PCM-1 ~ East of Taiwan PN ~ East China Sea TK ~ Tokara Strait south of Kyushu PCM-5 (ASUKA) ~ South of Japan 34°N & 38°N ~ Southeast and East of Japan
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Near PCM1 ~ East of Taiwan WOCE: Mean volume transports during 1994/9-1996/5 were estimated to be 23.3 Sv with a standard error of 2.0 Sv. Max in July-August and Min in October. Liu et al’s (1998): Mean transport estimate of 22.6 Sv from repeat CTD/ADCP sections. Johns et al, (2001): 21.5 Sv with an uncertainty of 2.5 Sv. Year 37-39, 5-day running mean
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W. E. Johns et al., (2001) Temporal Mean during Year 37-39. Position & Magnitude Mean downstream velocity structure during Sep 1994–May 1995. Depth & Magnitude Near PCM1 ~ East of Taiwan
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Near PN ~ East China Sea Oceanographic Division, Nagasaki Marine Observatory, JMA The long-term mean relative transport from 1973 to 2000 is 25.8 Sv with a mean seasonal maximum of 27 Sv in summer and minimum of 23.9 Sv in autumn. Year 37-39, 5-day running mean
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CPIES+ADCP observation during October 2003 until November 2004. M. Andres et al. (2008) Temporal Mean during Year 37-39. E. Oka et al. (2003) Quarterly data of CTD and shipboard ADCP from 1987 to 1997. Near PN ~ East China Sea
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Near TK ~ Tokara Strait South of Kyushu Observation from spring 1987 to spring 2005 and many estimates of the Kuroshio volume transport through Tokara Strait ranges from 18 Sv to 32 Sv (Bingham and Talley 1991; Yamamoto et al., 1993; Nakano et al., 1994; Yamamoto et al., 1998; Feng et al., 2000; Zhu et al., 2006). Year 37-39, 5-day running mean
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Near TK ~ Tokara Strait South of Kyushu
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E. Oka et al. (2003) Near TK ~ Tokara Strait South of Kyushu Year 37 Sep. Year 38 Jun. Year 39 Sep. 40 observations during 1987–97: 35/40 double current cores 25 Stronger northern core (Type 1) 10 Stronger southern core (Type 2) 5/40 single southern core (Type 3). There is no case of a single northern core.
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Volume Transport PCM-1 PN TK
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Three Typical Path of the Kuroshio M. Kawabe (2005) Non-large meander near-shore path Non-large meander off-shore path Large meander path
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Kuroshio Path Year 37 Sep. Year 38 Jun. Year 39 Sep. Non-Large Off-shore Meander Non-Large Meander Transition (Off to Near) Non-Large Near-shore Meander
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