Abstract
Climatological estimates for the values of static stability parameter are presented for the different pressure layers in the African atmosphere during the months of January, April, July and October. These values show very small variations on isobaric layers. In the vertical, the static stability values change rather rapidly so that the values for the 850–700 mb layer are, in all the four months, about three orders of magnitude less than those for the 50-30 mb layer.
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 callMore From: Archives for Meteorology, Geophysics, and Bioclimatology Series A
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.
