Abstract
Calculated insolations of the Earth are analyzed. The main trends in the modern solar climate change are identified: increased latitudinal contrast and smoothed seasonal differences. The correlation of the meridional insolation gradient with the average annual energy transfer in the ocean–atmosphere system is revealed. The features of changes in the annual and semiannual meridional insolation gradients and the correlation of latitudinal regions of maximum changes with the spatial localization of circulation cells (Headley, Ferrel, and Polar cells) and the regions in which vortex formations are generated and developed (tropical and extratropical cyclones) are revealed. The possibility of a link of between the decrease in the inclination of the Earth’s rotation axis and an increase in the meridional insolation gradient with an increase in climate turbulence is noted.
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.
