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.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
