Abstract
Most of the fundamental equations in fluid dynamics can be derived from first principles in either a Lagrangian form or an Eulerian form. Lagrangian equations describe the evolution of the flow that would be observed following the motion of an individual parcel of fluid. Eulerian equations describe the evolution that would be observed at a fixed point in space (or at least at a fixed point in a coordinate system such as the rotating Earth whose motion is independent of the fluid). If S(x, t) represents the sources and sinks of a chemical tracer Ψ(x, t) the evolution of the tracer in a one-dimensional flow field may be alternatively expressed in Lagrangian form as
, or in Eulerian form as
.
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According to the discussion in Section 2.3.2, the global truncation error is of same the order as the leading-order errors in the numerical approximation to the differential form of the governing equation (6.6) and is one power of Δt lower than the truncation error in the integrated form (6.5).
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© 1999 Springer Science+Business Media New York
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Durran, D.R. (1999). Semi-Lagrangian Methods. In: Numerical Methods for Wave Equations in Geophysical Fluid Dynamics. Texts in Applied Mathematics, vol 32. Springer, New York, NY. https://doi.org/10.1007/978-1-4757-3081-4_6
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DOI: https://doi.org/10.1007/978-1-4757-3081-4_6
Publisher Name: Springer, New York, NY
Print ISBN: 978-1-4419-3121-4
Online ISBN: 978-1-4757-3081-4
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