Abstract
The results of an analysis of the annual variation of the planetary boundary layer (PBL) height in the continent-ocean transition zone determined from lidar and meteorological data are presented. Means of the height and its variances are calculated in a month-long window. The PBL heights reconstructed from these measurements are found to differ substantially in the spring and summer seasons. These results are explained by the influence of dust storms and cyclones, which are the most intense in these seasons, on the structure of aerosol in the atmosphere.
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.
