Abstract
A one-dimensional mathematical model is proposed to describe thermal stratification in lakes. The vertical diffusion coefficient is formulated in terms of wind velocity and the gradient Richardson number. Heat exchange through the air-water interface can be calculated from the observed daily averaged meteorological data. This model is validated for simulation of temperature field observed in Lake Chuzenji. Calculated results of the thermal structure of the lake showed good agreement with the observed data. Effect of wind velocity on the thermocline formation is also evaluated.
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.