Note on the Theory of Land and See Breeze

Abstract

The theory of land and see breeze has aleady been attacked by various authors with some success in their respective manners. Here the present author also treated this problem from a little different stand-point of view. By properly omitting unnecessary terms in their magnitudes in the equations of motion, continuity and heat conduction, the author solved them, putting the distribution of temperature at the surface in the form; The result of our solution shows that the coefficients of kinematic eddy viscosity and eddy thermal diffusivity will have the numerical values ranging from 10⁸ to 10⁹, in their most, in C. G. S. units, which will be admissible in consideration of the scale of the influence domain of motion.