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dc.contributor.authorShayo, GR
dc.contributor.authorKiangi, PMR
dc.contributor.authorPatnaik, JK
dc.date.accessioned2015-07-17T11:55:45Z
dc.date.available2015-07-17T11:55:45Z
dc.date.issued1981
dc.identifier.citationArchives for meteorology, geophysics, and bioclimatology, Series A 1981, Volume 30, Issue 3, pp 197-209en_US
dc.identifier.urihttp://link.springer.com/article/10.1007/BF02257843
dc.identifier.urihttp://hdl.handle.net/11295/88106
dc.description.abstractClimatological 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.en_US
dc.language.isoenen_US
dc.publisherUniversity of Nairobien_US
dc.titleSome aspects of atmospheric static stability parameter of the atmosphere over Africa during the different major seasonsen_US
dc.typeArticleen_US
dc.type.materialenen_US


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