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Studies of convection in geophysical flows constitute an advanced
and rapidly developing area of research that is relevant to
problems of the natural environment. Since the late 1980s,
significant progress has been achieved in the field as a result of
both experimental studies and numerical modelling. This led to the
principal revision of the widely held view on buoyancy-driven
turbulent flows comprising an organized mean component with
superimposed chaotic turbulence. An intermediate type of motion,
represented by coherent structures, has been found to play a key
role in geophysical boundary layers and in larger scale atmospheric
and hydrospheric circulations driven by buoyant forcing. New
aspects of the interaction between convective motions and rotation
have recently been discovered and investigated at the end of the
20th century. Extensive experimental data have also been collected
on the role of convection in cloud dynamics and microphysics. New
theoretical concepts and approaches have been outlined regarding
scaling and parameterization of physical processes in
buoyancy-driven geophysical flows. The book summarizes
interdisciplinary studies of buoyancy effects in different media
(atmosphere and hydrosphere) over a wide range of scales (small
scale phenomena in unstably stratified and convectively mixed
layers to deep convection in the atmosphere and ocean), by
different research methods (field measurements, laboratory
simulations, numerical modelling), and within a variety of
application areas (dispersion of pollutants, weather forecasting
and hazardous phenomena associated with buoyant forcing).
Based on his over forty years of research and teaching, John C.
Wyngaard's textbook is an excellent up-to-date introduction to
turbulence in the atmosphere and in engineering flows for advanced
students, and a reference work for researchers in the atmospheric
sciences. Part I introduces the concepts and equations of
turbulence. It includes a rigorous introduction to the principal
types of numerical modeling of turbulent flows. Part II describes
turbulence in the atmospheric boundary layer. Part III covers the
foundations of the statistical representation of turbulence and
includes illustrative examples of stochastic problems that can be
solved analytically. The book treats atmospheric and engineering
turbulence in a unified way, gives clear explanation of the
fundamental concepts of modeling turbulence, and has an up-to-date
treatment of turbulence in the atmospheric boundary layer. Student
exercises are included at the ends of chapters, and worked
solutions are available online for use by course instructors.
Based on his over forty years of research and teaching, John C.
Wyngaard's textbook is an excellent up-to-date introduction to
turbulence in the atmosphere and in engineering flows for advanced
students, and a reference work for researchers in the atmospheric
sciences. Part I introduces the concepts and equations of
turbulence. It includes a rigorous introduction to the principal
types of numerical modeling of turbulent flows. Part II describes
turbulence in the atmospheric boundary layer. Part III covers the
foundations of the statistical representation of turbulence and
includes illustrative examples of stochastic problems that can be
solved analytically. The book treats atmospheric and engineering
turbulence in a unified way, gives clear explanation of the
fundamental concepts of modeling turbulence, and has an up-to-date
treatment of turbulence in the atmospheric boundary layer. Student
exercises are included at the ends of chapters, and worked
solutions are available online for use by course instructors.
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