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

M. Koizumi-1956-01-01-Papers in Meteorology and Geophysics

TL;DRAbstract

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.

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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.

Keywords

OceanographyClimatologyPacific oceanVariation (astronomy)Environmental scienceAtmospheric pressureGeologyPhysics

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