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Physics of Lakes - Volume 3: Methods of Understanding Lakes as Components of the Geophysical Environment (Hardcover, 2014 ed.)
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Physics of Lakes - Volume 3: Methods of Understanding Lakes as Components of the Geophysical Environment (Hardcover, 2014 ed.)
Series: Advances in Geophysical and Environmental Mechanics and Mathematics
Expected to ship within 12 - 17 working days
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The ongoing thread in this volume of Physics of Lakes is the
presentation of different methods of investigation for processes
taking place in real lakes with a view to understanding lakes as
components of the geophysical environment. It is divided into three
parts. Part I is devoted to numerical modeling techniques and
demonstrates that (i) wind-induced currents in depth-integrated
models can only adequately predict current fields for extremely
shallow lakes, and (ii) that classical multi-layered simulation
models can only adequately reproduce current and temperature
distributions when the lake is directly subjected to wind, but not
the post-wind oscillating response. This makes shock capturing
discretization techniques and Mellor-Yamada turbulence closure
schemes necessary, as well as extremely high grid resolution to
reduce the excessive numerical diffusion. Part II is devoted to the
presentation of principles of observation and laboratory
experimental procedures. It details the principles of operation for
current, temperature, conductivity and other sensors applied in the
field. It also discusses the advantages and limitations of common
measuring methods like registration from stationary or drifting
buoys, sounding and profiling from a boat, etc. Questions of data
accuracy, quality, and reliability are also addressed. The use of
laboratory experiments on a rotating platform is based on an
exposition of dimensional analysis and model theory and illustrated
using Lake Constance as an example. Part III gives an account of
the dynamics of lake water as a particle-laden fluid, which,
coupled with the transport of the bottom sediments, leads to
morphodynamic changes of the bathymetry in estuarine and possibly
whole lake regions. An elegant spatially one-dimensional theory
makes it possible to derive analytic solutions of deltaic
formations which are corroborated by laboratory experiments. A full
three-dimensional description of the evolution of the alluvial
bathymetry under prescribed tributary sediment input indicates a
potential subject for future research.
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