Researches on the Variations of Oceanographic Conditions in the Region of the Ocean Weather Station “ Extra ” in the North Pacific Ocean (VI)

A Note on the Diurnal Variation of Air Temperature on the Open Sea

Abstract

The swelling in the forenoon appearing in the diurnal variation curve of air temperature at Ocean Weather Stations “ Extra ” (39°N,153°E) and “ Tango ” (29°N,135°E), described in detail in the fourth of the author's present series of studies [1], may pretty well be explained by considering an adiabatic change due to the diurnal variation of atmospheric pressure.