Abstract
This memior is essentially a sequel to one whic one of the authors published lately in this journal. Intergrating Rayleigh's well-known thermohydrodynamical equations (Scientific Papers, Vol. VI, p. 436), the main characteristics of land and sea breezes are deduced. Stream lines, and vertical distribution of the horizontal air-current associated with land and sea breezes owing to the nature of the coast line are shown in Figs. 1-3. There is a good agreement between the theory and observations, as we could expect in such computations.
