Abstract
A general linear model with dummy coded time intervals is proposed for the detection of short term seasonal variations and deseasonalized long term trends in atmospheric total column ozone from 1957 to 2015. Data from ground stations located in the northern mid-latitudes, the tropics, and Antarctica show seasonal cycles and long term declining trends in total ozone that differ according to latitude. The long term decline is weakest in the tropics and strongest in Antarctica. Some evidence of stabilization and recovery of ozone levels is found.
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.
