Effect of variations in net basin supply on lake levels and outflows

Starting from a simplified version of the water balance equation, it is shown how the levels and outflows from a open lake can be related to the magnitude and statistical characteristics of the annual net basin supply series, which is defined as the net inflow arising from tributary inflows, rainfal...

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Bibliographic Details
Published inHydrological processes Vol. 12; no. 4; pp. 559 - 573
Main Author Sene, K. J.
Format Journal Article
LanguageEnglish
Published West Sussex John Wiley & Sons, Ltd 30.03.1998
Wiley
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Summary:Starting from a simplified version of the water balance equation, it is shown how the levels and outflows from a open lake can be related to the magnitude and statistical characteristics of the annual net basin supply series, which is defined as the net inflow arising from tributary inflows, rainfall on the lake surface and the lake evaporation. Using the models, estimates are derived for the response time for several large open lakes in Africa and Asia. Also, the observed net basin supply series for three major lakes (Victoria, Malawi and Toba) are investigated in detail. It is suggested that, on an annual basis, the assumption of a random normally distributed series of net basin supply can provide a reasonable first guess for the equilibrium response of a lake and for the likely range of variation of levels. These estimates are likely to be useful in water resources assessments and for investigations of the effects of land use and climate change on lake levels. The effects of departures from this simplified approach are discussed and are illustrated with some practical examples. © 1998 John Wiley & Sons, Ltd.
Bibliography:ark:/67375/WNG-W64632K7-Z
ArticleID:HYP594
NERC
istex:CF3D62B672529E528FACDF156745ABB6D1DD4017
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0885-6087
1099-1085
DOI:10.1002/(SICI)1099-1085(19980330)12:4<559::AID-HYP594>3.0.CO;2-R