Theoretical and Numerical Studies of Atmospheric Boundary-layer Flows Over Complex Terrain PDF Download
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Author: Marco Giovanni Giometto
Publisher:
ISBN:
Category :
Languages : en
Pages : 113
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Book Description
Mots-clés de l'auteur: anabatic flow ; direct numerical simulation ; dynamic surface roughness model ; energy budget ; immersed boundary method ; katabatic flow ; large-eddy simulation ; Prandtl model ; rough surfaces ; turbulence.
Author: Marco Giovanni Giometto
Publisher:
ISBN:
Category :
Languages : en
Pages : 113
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Book Description
Mots-clés de l'auteur: anabatic flow ; direct numerical simulation ; dynamic surface roughness model ; energy budget ; immersed boundary method ; katabatic flow ; large-eddy simulation ; Prandtl model ; rough surfaces ; turbulence.
Author: Norman K. Wagner
Publisher:
ISBN:
Category : Boundary layer (Meteorology)
Languages : en
Pages : 179
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Book Description
Author: Massimiliano Burlando
Publisher:
ISBN:
Category :
Languages : en
Pages : 192
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Book Description
Author: Demetri P Lalas
Publisher: World Scientific
ISBN: 9814602833
Category :
Languages : en
Pages : 768
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Book Description
This volume is a collection of lectures given at the two colloquia on atmospheric flows over complex terrain with applications to wind energy and air pollution, organized and sponsored by ICTP in Trieste, Italy. The colloquia were the result of the recognition of the importance of renewable energy sources, an important aspect which grows yearly as the environmental problems become more pronounced and their effects more direct and intense, while at the same time, the wise management of the Earth's evidently limited resources becomes imperative.It is divided into two main parts. The first, which comprises Chaps. 1 to 4, presents the structure of the atmospheric boundary layer with emphasis in the region adjacent to the ground. The second, Chaps. 5 to 10, discusses methods for the numerical computation of the wind field on an arbitrary terrain. The unique feature of this book is that it does not stop at the theoretical exposition of the analytical and numerical techniques but includes a number of codes, in a diskette, where the mechanisms and techniques presented in the main part are implemented and can be run by the reader. Some of the codes are of instructional value while others can be utilized for simple operational work.Some of the lecturers are: D N Asimakopoulos, C I Aspliden, V R Barros, A K Blackadar, G A Dalu, A de Baas, D Etling, G Furlan, D P Lalas, P J Mason, C F Ratto and F B Smith.
Author: J. R. Garratt
Publisher: Cambridge University Press
ISBN: 9780521467452
Category : Mathematics
Languages : en
Pages : 340
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Book Description
The book gives a comprehensive and lucid account of the science of the atmospheric boundary layer (ABL). There is an emphasis on the application of the ABL to numerical modelling of the climate. The book comprises nine chapters, several appendices (data tables, information sources, physical constants) and an extensive reference list. Chapter 1 serves as an introduction, with chapters 2 and 3 dealing with the development of mean and turbulence equations, and the many scaling laws and theories that are the cornerstone of any serious ABL treatment. Modelling of the ABL is crucially dependent for its realism on the surface boundary conditions, and chapters 4 and 5 deal with aerodynamic and energy considerations, with attention to both dry and wet land surfaces and sea. The structure of the clear-sky, thermally stratified ABL is treated in chapter 6, including the convective and stable cases over homogeneous land, the marine ABL and the internal boundary layer at the coastline. Chapter 7 then extends the discussion to the cloudy ABL. This is seen as particularly relevant, since the extensive stratocumulus regions over the subtropical oceans and stratus regions over the Arctic are now identified as key players in the climate system. Finally, chapters 8 and 9 bring much of the book's material together in a discussion of appropriate ABL and surface parameterization schemes in general circulation models of the atmosphere that are being used for climate simulation.
Author: Vallampati Ramachandra Prasad
Publisher: BoD – Books on Demand
ISBN: 1839681853
Category : Mathematics
Languages : en
Pages : 236
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Book Description
Written by experts in the field, this book, "Boundary Layer Flows - Theory, Applications, and Numerical Methods" provides readers with the opportunity to explore its theoretical and experimental studies and their importance to the nonlinear theory of boundary layer flows, the theory of heat and mass transfer, and the dynamics of fluid. With the theory's importance for a wide variety of applications, applied mathematicians, scientists, and engineers - especially those in fluid dynamics - along with engineers of aeronautics, will undoubtedly welcome this authoritative, up-to-date book.
Author: Nash'at Naveed Ahmad
Publisher:
ISBN:
Category : Atmospheric turbulence
Languages : en
Pages : 198
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Book Description
Author: Norman K. Wagner
Publisher:
ISBN:
Category :
Languages : en
Pages : 179
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Book Description
Three separate studies concerning flow over inhomogeneous terrain are presented. Two-dimensional nonlinear models were constructed and then integrated numerically. In the first study, the atmospheric boundary layer flow over terrain with a discontinuous variation in roughness was studied. A time dependent numerical model, using Blackadar's expression of mixing length and assuming no dynamic pressure effect and no vertical displacement of the zero velocity level at the lower boundary, was integrated until a steady-state situation was reached. The results agree with earlier theoretical work of Panofsky and Townsend and also with observations by Sterns and Lettau. The second study represents an attempt to solve a problem similar to the one just described using a steady-state model. An iterative method for solving the equations was derived. In addition, the dynamic pressure effect was also incorporated. The results show satisfactory agreement with those of Panofsky and Townsend. It is found that the dynamic pressure effect causes an apparent horizontal smoothing of the motion field. In the third study, the effect of an isolated hot surface (10 km wide) on the motion and temperature field is investigated. The model is time dependent and is based primarily on a sea breeze model by Estoque. As expected, the results show that the intensity of the upward motions which are induced is inversely proportional to the strength of the prevailing flow. The perturbations in both the temperature and velocity fields extend to several tens of kilometers downwind of the hot surface.
Author: Demetri P. Lalas
Publisher: World Scientific Publishing Company Incorporated
ISBN: 9789810225094
Category : Science
Languages : en
Pages : 753
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Book Description
Author: Yi Han
Publisher:
ISBN: 9781088395493
Category : Air flow
Languages : en
Pages : 172
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Book Description
The present work establishes a complete process to perform the micro-scale simulations of the neutral atmospheric boundary layer (ABL) flow over realistic terrain with multi-fidelity turbulence modeling approaches, and to validate the numerical predictions with the available on-site wind data. The complex terrain is located within the Chokecherry and Sierra Madre wind farm site which encompasses about 500 square kilometers of rugged and diverse terrain in south-central Wyoming. A robust conditional sampling procedure for the meteorological tower (met-tower) data to identify near-neutral ABL condition based on a criterion of the turbulence intensity is developed. The conditionally averaged wind data on fourteen met-towers is used for the model validation. The ABL flow simulations are conducted based on the OpenFOAM-based simulator for on/offshore wind farm applications (SOWFA) with both RANS and LES turbulence modeling approaches. The turbulent inflow is generated through a two-stage iterative approach using a precursor method. Appropriate boundary conditions are developed to adjust the real flow patterns over the complex terrain. In the RANS approach, a new formulation to calculate the production term in the transport equation for the turbulent kinetic energy (TKE) is developed to greatly reduce the commonly observed nonphysical near-surface TKE peak, and to improve the prediction of law-of-the-wall scaling in the near-surface region. In the LES approach, a low-dissipative, scale-selective discretization scheme is applied to the non-linear convection term of the filtered momentum equation. The aim is to reduce the numerical dissipation arising from the typically adopted upwind-biased schemes while maintaining second-order accuracy. The simulation results from both RANS and LES approaches are qualitatively compared with each other, and quantitatively compared to the conditional met-tower data in terms of the mean, standard deviation and direction of the wind at three about ground levels. The instantaneous flow field and turbulent structures are predicted by the LES approach. Overall, the wind statistic obtained by RANS and LES approaches show reasonable agreement compared to the met-tower data, except for some under-predictions at four met-tower located closer to the main ridge of the hill in a region of strong terrain variations.
