Transport and Mixing in Geophysical Flows

Häftad, Engelska, 2010

539 kr

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Beskrivning

Transports in fluids can be approached from two complementary perspectives. In the Eulerian view of mixing, the focus is on the concentration field. In the Langrangian view, fluid parcels are followed around as they move with the flow, experiencing chaotic or stochastic motion. This book examines both pictures, presenting a number of theoretical and experimental lectures on various aspects of transport and mixing of active and passive particles in geophysical flows.

Produktinformation

Utgivningsdatum:2010-11-30
Mått:155 x 235 x 15 mm
Vikt:417 g
Format:Häftad
Språk:Engelska
Serie:Lecture Notes in Physics
Antal sidor:262
Förlag:Springer-Verlag Berlin and Heidelberg GmbH & Co. KG
ISBN:9783642094484

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Recensioner i media

From the reviews: "The book contains original research articles by many of the world's leading researchers in geophysical fluid dynamics. ... I have read this book with great interest and pleasure. The style of presentation is clear and readable. ... this book will definitely help those who know the subject and who are interested in theoretical approaches, with a direct preference for the geophysical fluid dynamics. Graduate students of geophysics and applied mathematics interested in environmental fluid mechanics should also reference it." (Andrzej Icha, Pure and Applied Geophysics, Vol. 166, 2009)

Innehållsförteckning

Theory.- Scalar Decay in Chaotic Mixing.- Transport of Inert and Reactive Particles: Lagrangian Statistics in Turbulent Flow.- Diffusion and Reaction–Diffusion in Steady Flows at Large Péclet Numbers.- An Introduction to Radiative Transfer for Geophysicists.- Coherent Vortices and Tracer Transport.- Experiments and Observations.- Dispersion and Mixing in Quasi-two-dimensional Rotating Flows.- Quantifying Inhomogeneous, Instantaneous, Irreversible Transport Using Passive Tracer Field as a Coordinate.- Lagrangian Statistics from Oceanic and Atmospheric Observations.- The Modulation of Biological Production by Oceanic Mesoscale Turbulence.