104 The Three-dimensional Temperature Distribution and its Variation in Time 



{e) Horizontal Convection and Lateral Mixing 



The dynamic convection discussed in the preceding section applies only to mixing 

 of water masses in a vertical direction moving in a horizontal turbulent flow. In 

 addition to this vertical mixing process there will also be a mixing process, largely 



Table 41. Coefficients of eddy conductivity, eddy diffusivity and eddy viscosity 



Table 42. Advance of a sudden temperature change penetrating into the sea by thermal 

 turbulent conductivity {half value time of surface disturbance) 



