東京に於ける氣温の日變化に就いて
1938 年 16 巻 7 号 p. 288-290
詳細
1938 年 16 巻 7 号 p. 288-290
The effect of various meteorological elements on the diurnal variation of air temperature were calculated and it is found that, in winter the greatest effect is due to the eddy conduction from the surface both before and after sunset while in summer it is due to the latent heat of the evaporation from the surface before sunset and the eddy conduction of the air after sunset.
