Abstract
The concentration and daily variations in ozone concentration at ground level in Northern Greenland were measured. A correlation was found between sunlight and ozone concentration. This correlation, coupled with the knowledge of air-moss movements in the region, provides excellent evidence that the ozone being measured was formed continuously in the atmosphere and was not brought to the area by some transport mechanism. The results also indicate that ozone is a transient intermediate in the atmosphere and that it decomposes as fast as it forms.
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.
