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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Published in | Hydrological processes Vol. 12; no. 4; pp. 559 - 573 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
West Sussex
John Wiley & Sons, Ltd
30.03.1998
Wiley |
Subjects | |
Online Access | Get full text |
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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. |
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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 |