Abstract
Based on the principles of the hydrodynamic flow around a solid body, including rotating one, the mechanisms of convective storm evolution are considered. The origin of sources of the arrival of the resource to the storm, as well as the pattern of its assimilation are refined. The possibilities of the formalized indication of the storm propagation are shown.
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.
