Abstract
Interactions between oceanic heat transfer and the formation of the fields of spatial geopotential gradients in the middle troposphere has been studied using linear regressive analysis. The analysis of the spatial distribution of coefficients of correlation shows that heat fluxes in the Northern Atlantic play a significant role in the formation of circulation features of the middle troposphere over the Atlantic–European region, which indicates the possible predictability of large-scale characteristics of circulation due to oceanic processes.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.