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Christian Kharif. William G. Don Kulasiri. Andreas Fichtner. Home Contact us Help Free delivery worldwide. Hasegawa and F. Tappert, Transmission of stationary nonlinear optical pulses in dispersive dielectric fibres , I. Anoma- lous dispersion, Appl. Guo, L. Ling, and Q. E 85 , Bandelow and N. A , Tao , K. Porsezian , and A.

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Ankiewicz , Extreme waves that appear from nowhere: on the nature of rogue waves , Phys. Ismail , Classical and quantum orthogonal polynomials in one variable , Encyclopedia of Mathematics and its Applications, vol. Askey; Reprint of the original.

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The method provides dynamic equations for phases, interfaces, an. Gradually-varied flow GVF is a steady non-uniform flow in an open channel with gradual changes in its water surface elevation. The evaluation of GVF profiles under a specific flow discharge is very important in hydraulic engineering.

This book prop. The advection-dispersion equation that is used to model the solute transport in a porous medium is based on the premise that the fluctuating components of the flow velocity, hence the fluxes, due to a porous matrix can be assumed to obey a relationsh. The formation of internal waves requires seasonal stratification of the water bodies and generati.

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Soil is matter in its own right. Its nature can be captured by means of monotonous, cyclic and strange attractors. Thus material properties are defined by the asymptotic response of sand- and clay-like samples to imposed deformations and stresses. A three-tier approach is presented: i fundamental dynamical concepts of climate processes, ii their mathematical formulation based on balance equations, and iii the necessary numerical techniques to solve these equations. This book showcase. This first volume in the treatise on the Physics of Lakes deals with the formulation of the mathematical and physical background.

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Full waveform tomography is a tomographic technique t.