Abstract
Recently revised estimates for the photochemical loss rates of tropospheric OCS indicate that ocean hydrolysis may be the most important sink. A simple air→sea thin film transfer model, coupled with water hydrolysis indicates that the lifetime of tropospheric OCS with respect to this flux has a lower‐limit of 11 years, which yields a net lifetime for tropospheric OCS of 4‐7 years.
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.
