Abstract
Consecutive Landsat images of a red clay turbidity plume due to runoff from Nemadji River, Wisconsin, are used in computation of the horizontal eddy diffusivity for Lake Superior. Dispersion of turbid areas ranging from 2.5-5.4 km in diameter and having average velocities of 0.4 cm/sec-6.1 cm/sec are investigated. The coefficient for horizontal eddy diffusivity ranges from 0.6-1.5 m 2/sec.
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.
