Abstract
Results of experimental investigations and a theoretical estimation of the polar conductivity profiles in the turbulent surface layer over flat ground are discussed. The results presented are evidence for the occurrence of the steady electrode effect over land. By reducing the number of factors which influence the vertical conductivity profile and applying a special measuring technique, it has been possible to obtain steady profiles. The experimental results are in good agreement with the hypothesis of a turbulent electrode effect in the boundary of strong turbulent mixing. The agreement implies the confirmation of the relation between the surface wind, the electrical conductivity and the thickness of the electrode-effect layer.
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.
