Abstract
An algorithm for computation of the parameters of a quasi-stationary barotropic planetary boundary layer (PBL) IS discussed. On the basis ~f the results of a number of numerical experiments, relations between the observed meteorological fields and the Internal parameters of the PBL have been established. A method is proposed to parameterize eddy momentum flux and frictional vertical velocity for their use in multi-level primitive equations (PE) 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.
