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A three dimensional-circulation model of Lake Tanganyika

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Part of the book series: Developments in Hydrobiology ((DIHY,volume 141))

Abstract

A combination of field measurements and computer modelling was selected as a main approach, when the Hydrological Subcomponent of the Lake Tanganyika Research (LTR) Program was established. The main goal of the modelling work is to estimate the role of main factors affecting water currents in Lake Tanganyika and to understand the peculiarities of spatial and temporal variations of its hydrophysical characteristics. Special attention is given to a more accurate description of wind-induced shear stresses, the main driving force of the lake dynamics. Numerical experiments with a mesoscale meteorological model show the significant role of a coastal diurnal slope-lake breeze system, intensified during the dry season while south-easterly trade winds supply the main amount of energy to the middle of the lake.

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© 1999 Springer Science+Business Media Dordrecht

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Podsetchine, V., Huttula, T., Savijärvi, H. (1999). A three dimensional-circulation model of Lake Tanganyika. In: Lindqvist, O.V., Mölsä, H., Salonen, K., Sarvala, J. (eds) From Limnology to Fisheries: Lake Tanganyika and Other Large Lakes. Developments in Hydrobiology, vol 141. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-1622-2_2

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  • DOI: https://doi.org/10.1007/978-94-017-1622-2_2

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-90-481-5339-8

  • Online ISBN: 978-94-017-1622-2

  • eBook Packages: Springer Book Archive

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