The water balance of Lake Victoria

Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/352

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DC Field	Value	Language
dc.contributor.author	Piper, B.	-
dc.contributor.author	Plinston, D.	-
dc.contributor.author	Sutcliffe, J	-
dc.date.accessioned	2018-09-25T14:56:33Z	-
dc.date.available	2018-09-25T14:56:33Z	-
dc.date.issued	1986	-
dc.identifier.citation	Hydrological Sciences - Journal Vol.31,p.1,3	en_US
dc.identifier.uri	http://hdl.handle.net/123456789/352	-
dc.description.abstract	The sharp rise in the level of Lake Victoria between 1961 and 1964 has been found difficult to explain in terms of the components of the water balance. After reviewing lake inflows and the method of calculating lake rainfall from lakeside gauges, the historic lake water balance has been reproduced. The rise in lake level can be explained through rainfall and resulting tributary inflows, which would allow projections of possible future levels to be made by analysis of rainfall series.	en_US
dc.language.iso	en	en_US
dc.publisher	Taylor & Francis	en_US
dc.subject	level	en_US
dc.subject	Lake Victoria	en_US
dc.subject	water balance	en_US
dc.subject	lake rainfall	en_US
dc.subject	water balance	en_US
dc.subject	inflows	en_US
dc.title	The water balance of Lake Victoria	en_US
dc.type	Article	en_US
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