Abstract
The budget methods and the mixed layer model used to analyze the aircraft data from the First ISLSCP Field Experiment (FIFE) are outlined. The separation of the temporal and horizontal derivatives is discussed. Vector budgets for the mixed layer are presented on conserved variable diagrams. Theoretical solutions are given for the critical surface Bowen ratio, which produces no boundary layer moistening or equivalent potential temperature rise as a function of the Bowen ratio at the inversion. Improved measurement strategies are suggested.
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.
