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(1998). <i>Proceedings of the Second International Conference on Tropical Climatology, Meteorology and Hydrology, Brussels, 13-14 December 2001.</i> pp. 27-40","BEntID":100036,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Demarée, G.R. <i>et al.</i> (1998). <i>Proceedings of the Second International Conference on Tropical Climatology, Meteorology and Hydrology, Brussels, 13-14 December 2001.</i> pp. 27-40","DocTypID":17,"DocType":"Book chapters","MarineFlag":0,"FreshFlag":1,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Naithani, J.; Deleersnijder, E.; Plisnier, P-D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Naithani, J.; Deleersnijder, E.; Plisnier, P-D.","Englishabstract":"A two-dimensional, reduced gravity model is established to study the wind-induced oscillations of the thermocline of Lake Tanganyika. An analytical solution is obtained for a simplified, one-dimensional, linearized set of equations, which suggests that the first mode of oscillation - exhibiting one node only - should be dominant. The sensitivity to the wind stress, the stratification and the unpertubed thermocline depth of the amplitude and period of t he linear solution is analysed. 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