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Figure9. the solution to problems T1+T2+T3 for (a) λ=0, (b)λ=1 

Figure9. the solution to problems T1+T2+T3 for (a) λ=0, (b)λ=1 

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Figure8. í µí°“ í µí¿í µí¿’ field in a meridional section. (a) λ=0,...
Figure9. the solution to problems T1+T2+T3 for (a) λ=0, (b)λ=1 
Figure10-the solution to problems T 1 +T 2 +T 3 +T 4 for (a) λ=0, (b)λ=1 
Figure 11-the solution to problems T 0 +T 1 R 0 E-1 
Investigation of Water Circulation And Temperature Effect In Indian Ocean By Perturbation Method
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The tropical Indian Ocean forms the major part of the largest warm pool on Earth, and its interaction with the atmosphere plays an important role in shaping climate on both regional and global scales. Three dimensional temperature and velocity fields are calculated analytically for an ocean forced by wind stress and surface heat flux. A basic therm...
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