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

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.

More than Skin Deep: Sea Surface Temperature as a Means of Inferring Atlantic Water Variability on the Southeast Greenland Continental Shelf Near Helheim Glacier

“…Diurnal biases cause a decoupling between the ocean skin and underlying water (Donlon et al, 2002;Minnett, 2003;Price et al, 1986). They are expected as a result of differences in diurnal thermocline and skin temperature effects on SST skin between day-and nighttime, which also vary seasonally (e.g., Eastwood et al, 2011;Koizumi, 1956;Sverdrup et al, 1942). We calculate the diurnal bias based on differences between the day-and nighttime products for SNOW ET AL.…”