Abstract
Abstract Empirical formulas which have been derived to describe the profiles of wind, temperature and humidity through the atmospheric surface boundary layer (SBL) are used to derive equations predicting the fluxes of momentum, heat and moisture through the SBL. These formulas can be applied in the computation of lower boundary conditions needed for the diffusion equation in planetary boundary layer models.
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.
