A modified reduced gravity model for interannual variations of a sub-tropical ocean
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[1] B. Qiu,et al. Interannual variability in the mid- and low-latitude western North Pacific , 1992 .
[2] M. Darby,et al. Nonlinear Rossby waves in a thermodynamic reduced gravity ocean , 1990 .
[3] Syukuro Manabe,et al. Transient Response of a Global Ocean-Atmosphere Model to a Doubling of Atmospheric Carbon Dioxide , 1990 .
[4] D. Stevens. On open boundary conditions for three dimensional primitive equation ocean circulation models , 1990 .
[5] Howard P. Hanson,et al. Mixed Layer-Thermocline Interaction in a Three-Dimensional Isopycnic Coordinate Model , 1989 .
[6] M. A. Rennick,et al. Comments on “Slowly Propagating Disturbances in a Coupled Ocean-Atmosphere Model” , 1986 .
[7] R. Haney. Midlatitude sea surface temperature anomalies: a numerical hindcast , 1985 .
[8] David L. T. Anderson,et al. Slowly Propagating Disturbances in a Coupled Ocean-Atmosphere Model , 1985 .
[9] R. Hughes. On the equatorial mixed layer , 1980 .
[10] R. Haney. Surface Thermal Boundary Condition for Ocean Circulation Models , 1971 .
[11] R. Dickson,et al. A recurrent and persistent pressure-anomaly pattern as the principal cause of intermediate-scale hydrographic variation in the European shelf seas , 1971 .
[12] H. Stommel,et al. The westward intensification of wind‐driven ocean currents , 1948 .
[13] P. K. Kundu,et al. A numerical investigation of dynamics, thermodynamics and mixed-layer processes in the Indian Ocean , 1993 .
[14] J. Woods. Chapter 34 The physics of Thermocline Ventilation , 1985 .