Abstract
Observations of fogs at Misawa Fishing Port in the Aomori district were made with a tethered balloon system and a doppler sodar system from 15 June to 11 July in 1993. Minute analyses were made of time changes of fogs for a long period from the evening on 7 July to the next noon and for a short period from 6 to 13JST on July. The results show that the atmosphere at the cloud top becomes stable from the view point of CTEI (cloud-top entrainment instability) about 2 hours before the intrusion of the fog and becomes neutral (or unstable) just before fog dissipation.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
More From: Journal of the Meteorological Society of Japan. Ser. II
Disclaimer: 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.